Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

Limbus

Sunsets~EXPLORE 7-27-08 #404

Please view LARGE if you have a moment. The bottom portion is the ocean.

This sculpture called "Angel" hangs at Ruth's Parkside Cafe. It was created by Jay Bolotin for his work called Limbus, a Mechanical Opera. His studio was located in the repurposed American Can Company Building as is Ruth's Parkside Cafe. The sculpture was sold to the cafe in exchange for a piece of pie.

Northside, Cincinnati. Keep Northside weird.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

This simple undressed stone monument is located in a beautiful setting near Mulranny, on the shores of the Atlantic Ocean (Clew Bay is just beyond the sand dunes here); with Croagh Patrick in the background. It marks a childrens’ burial ground, or cillín.

Until relatively recent times the Catholic Church would not allow children who were unbaptised at the time of their death to be buried in consecrated ground. It held that baptism was the necessary threshold through which all must pass before entering Christian society, and so have any possibility of getting to heaven. A more barbaric, uncaring and un-Christian approach I cannot imagine, forcing as it did parents to bury dead babies wherever they would, or could, but not in consecrated ground. This where, in the West of Ireland in particular, we had a society where there were no other official graveyards and where infant mortality rates were exceptionally high.

I understand that the current position of the Catholic Church is that the notion of Limbus Infantus, or what is more commonly called Limbo, has never been dogmatically defined. However, in the past, the approach of the Catholic Church in Ireland was nothing if not dogmatic on this point. As a result we have cillíni scattered all over the rural landscape of the West of Ireland, and in Mayo in particular.

In recent years local communities have in very many cases erected simple memorials, like this one at Mulranny, to remember those buried there. It is good that we remember them.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

The man is in nepali hat (topi, Dhaka topi) and the woman has typical Limbu ornaments. See Wikipedia article about Limbu people.

Close to my house is a cart that belongs to the Bandra Bazar IceGolawala..who sells Ice Golas and Limbu Pani, or lime sherbet..an array of bottles with colored essence.

Our Bandra Bazar Road Ice Gola wala is a UP Bhaiyya ..from North India a maligned lot due to parochial politics of self gain and convenience...but he shows no sign of regret.. he is a part of a childs growing up.. from one generation to the next.

Be it Fred in Texas or me or my kids we have tasted the ice gola after a hectic game of cricket.

Now one day another Ice Golawala backed by the local hoodlums , muscled in and threw our Ice golawala out from his regular space , the poor guy moved on to a side lane that is extremely hot without shelter, but his clientele did not leave him, they followed him here.

In the mean time the new Icegolawala had no business and finally deserted his post, the locals bought the old guy back.

In all this stress our Ice golawala cut his palm very badly on the ice shaving machine on the cart, I told him to take a septic shot and dressed his wound every day at my house.

His hand healed , and he has great respect for me loves Marziya.. though we dont eat ice golas or drink ice lime sherbet.Mind you he is clean hygienic.. but I cant take chances with Marziya..

Instead I shot some frames and told him, that he is going to be seen by everyone in the world..a thought that made him happy..

Now because the hot shot media photographer wont highlight stories of the Am Admi the common man God created the photo blogger and blessed him with a pedestrian humility too.. that with due respect to Fred Miller I have tagged as street photography..

And on a second thought without Fred Miller I might have been lost in the woods..he is there helping us out with new stuff, it was Fred who recommended me to Now Public...an experience that has come in handy in learning the ways of the world.. had I posted this story at Now Public..it would have been flagged either by Jarrett or Tina Kellis..erstwhile editors, as not being up to the mark, they would question, what is so news worthy about this story, and this is a fact ..a bias exists for the colored man in a white mans world..do read our terms and guidelines on posting a new story..

Jarrett Martineau

at 08:27 on March 19th, 2009

Thanks for the post, firozeshakir, we're glad you're enjoying contributing to NowPublic. Although your poem is appreciated, we do encourage our members to post newsworthy stories to the site. If you haven't done so, check out our Contributor Guidelines for more help posting news stories to the site.

blah blah ha ha ha ...

But than Fred would recommend this story so would Nauman , or Cypresso or Esta or Uwe..not because of its newsworthiness because it is a tale of a child's happiness costing Rs 1.. the price of a icegola or the lime sherbet.. cheaper than the newspaper too.. in Mumbai.

optional title News / Blogs

Overcast evening during twilight from the deck of Limbus Restobar, probably the restaurant with the best view in Cusco.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Sunsets

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

APC . B57 . ATLR. - Limbus

Atlatlahucán 2013.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Una tormenta mas y en toda su extensión por encima de las Sierras que rodean a la ciudad Capital de San Luis. Apenas un destello de un rayo anuncia su llegada. //

A storm and at length over the Sierras that surround the capital city of San Luis. Just a flash of lightning announces its arrival.

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GLS Nikon D300 / Sigma 17-70mm f/2.8 DC Macro HSM /

www.glsfotografia.com.ar/

www.fotosensor.com.ar/

www.sanluisnatural.net/

-----------------------------------------------------------------------------------------------------

Mt Kanchenjunga is the 3rd highest peak in the world after Mt Everest and K2. Some even consider this to be the 2nd Highest Peak in the world over K2 but the matter is yet to be settled, Kangchenjunga is called Sewalungma in the local Limbu language, translates as 'Mountain that we offer Greetings to'.

The picture is taken from Tiger Hill Observatory in Darjeeling, West Bengal,India.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Experimenting with a macro lens and side lighting through an eyeball reveals the multiple strands of papillary dilator & constrictor muscles, showing that the beautiful iris can actually be somewhat creepy when viewed too closely. The small lines and colors we notice within an iris are individual muscle strands used to pull the pupil open or closed. And layers of the corneal limbus appear as flawed ledges having jagged drop-offs around the exterior of the cornea, easily identified once lighting is angled across the eye.

This image is best viewed at it's largest size (1024px). Lighting was a 200w/s studio light thru gridded snoot, placed to the far left of subject's face (camera-right) to limit reflections. Canon 50mm f2.8 Macro lens on Canon 5D-MII.

Watch the video @ youtu.be/EfZaTeNUtbY

Two two beautiful women make Nepal's traditional Dhaka fabric in a workshop behind their house. The daughter is studying to be a teacher but still weaves in her spare time after class. The father originally bought the family's looms in India and then made the punch hole cards to generate the traditional patterns found in Dhaka cloth.

In many parts of central Nepal, women weave Dhaka fabric in their spare time. Traditionally it originates with the Limbu people of eastern Nepal, who don't used a punch-card loom, seen here. Now-a-days Dhaka fabric is used mainly for sewing "topi", the traditional Nepali men's hat. It used to be more commonly used also for making men's vests and women's blouses (a dhaka-ko-cholo).

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The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

238,120 items / 1,998,996 views

My last meeting with Sir was at Lilavati and as a person who knew Mr Rajesh Khanna since his Sauten days , than there was a huge gap, and I met Mr Rajesh Khanna in the aircraft years later I was wearing a newspaper suit a copy of the same suit that I had made for Govinda in Gambler for his hit song Meri Marzi and now I was wearing the newpaper suit for the premiere of Eena Mena Deeka a film starring Rishi Kapoor Vinod Khanna and directed by David Dhawan who was in this chartered aircraft too.. and I was working with Mr Nitin Manmohan producer the banner Neha Arts, the most eponymous that give hits like Bol Radha Bol Insaf Mahasangram.

Mr Rajesh Khanna was the guest for the premiere and once upon a time very close to Manji or Mr Manmohan a great villain his best friend and father of Nitin Manmohan my boss and Hemant Panchmiya his elder brother .

He was fascinated with my look and as we knew each other he told me to look me up in Mumbai and I did.

I began doing sirs clothes after the untimely death of designer Moez but I did his clothes as a goodwill gesture and to learn something from him.

I did the look of his incomplete film by Ashok Tyagi and Vijay Sirohi DonKe Bad Kaun.. this was the tme I got very close to Sir his moods his nostalgia d his trips down Bollywood memory lanes.

When he was going for the family reunion with Akshay Kumar and the rest of his family to Goa he made me make a few Bermuda shorts and a few jeans he was happy like a child that has found his favorite lost toy.

Than he met my grand daughter Marziya Shakir on Bakra Eid and she added a missing joy to his person , she became his grand child too, he pampered her with chocolates and told her stories I shot these private moments and shared it with people on the net.

Than I finally did the black tuxedo for Balkis Havells fan ad, he had insisted he did not want me to change his old measurements , I politely told him ,it would not work, he had lost oodles and his framework had metamorphosed but all he said make the trousers Duck Style adding 3 extra buttons I did.

The pleated shirt was too huge on him so I made him a new one.. and could hardly do anything to the Tuxedo..from collar size 16.5 he had become 14 after his illness and swollen feet, but he did the fittings and and as the Unit and direction took his video I shot his stills as my collection of memories.

After the left we both cried .. he had pulled it off with aplomb.. and Bala his trusted Man Friday bought me thanda limbu pani.

After he came back from the shoot he called me told me to bring my grand kids.. but he was seriously disturbed , and I thought of going away my little one Nerjis Asif Shakir had just learnt to walk, Marziya Shakir 4 years normally shot his pictures too on my camera but seeing the change I hastily fled he blessed my grand kids and that was the last time.

So I was not ready to brave the rains and follow the cavalcade the funeral cortege going to the crematorium I did not want to document his last journey from home .. for me he is still at home a lonely man living with his fame his illusions his dreams and the poetry of his life.

Yes he loved me a lot. He loved my grand kids a lot.

Legends dont die they leave their fooprints on the sands of Time.

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Somewhere in ruins, there is a hope, in form of nice flower.

HBW to all Flickr friends, and guests!

Photo was taken in ruins from one restaurant, near Limbus, not far from river Drava. Fire destroyed the place almoust completly. Sad.

All my images are copyrighted.

If you intend to use any of my pictures, for any usage, you need to contact me first.

Thank you.

St. Andrew's Church, Darjeeling. Built- 1843, Rebuilt- 1873

Darjeeling is a town and a municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,042.2 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal.

The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognised and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract pupils from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighbouring town of Kalimpong, was a centre of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanisation.

TOPONOMY

The name Darjeeling comes from the Tibetan word dorje, meaning the thunderbolt sceptre of the Hindu diety Indra, and ling, a place or land.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the River Mechi and the River Teesta to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2. During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district. Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.[

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,000 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen.

The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.

Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIL ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden. Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2 The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.

From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results.

The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger.

Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away. The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour. Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1,005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent.

According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English.

Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination.The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme.

A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk. Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life.

Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent and St. Paul's School are renowned as centres of educational excellence.

Darjeeling has four colleges — St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College — all affiliated to the University of North Bengal in Siliguri.

WIKIPEDIA

EXPLORE 9-23-08 #371

Yes, star crossed in pleasure, the stream flows on by

Yes, as we're sated in leisure, we watch it fly

And time waits for no one, and it won't wait for me

And time waits for no one, and it won't wait for me

Time can tear down a building or destroy a woman's face

Hours are like diamonds, don't let them waste

Time waits for no one, no favours has he

Time waits for no one, and he won't wait for me

Men, they build towers to their passing yes, to their fame everlasting

Here he comes chopping and reaping, hear him laugh at their cheating

And time waits for no man, and it won't wait for me

Yes, time waits for no one, and it won't wait for me

Drink in your summer, gather your corn

The dreams of the night time will have vanished by dawn

And time waits for no one, and it won't wait for me

And time waits for no one, and it won't wait for me

No no no, not for me....

by M. Jagger/K. Richards

From Hee Gaon, West Sikkim.

Location of peak: 27° 42' N; 88° 9' E

Location of Hee Gaon: 26º 4’ and 28º 7’48” N; 86º’ and 88º 55’25” E

Kangchenjunga (Nepali:कञ्चनजङ्घा Kanchanjaŋghā) SewaLungma (Limbu language) is the third highest mountain in the world (after Mount Everest and K2), with an elevation of 8,586 metres (28,169 ft). Kangchenjunga translated means "The Five Treasures of Snows", as it contains five peaks, four of them over 8,450 metres. The treasures represent the five repositories of God, which are gold, silver, gems, grain, and holy books. Kangchenjunga is also called Sewalungma in local Limbu language and considered sacred in Kirant religion.

Three of these five peaks (main, central, and south) are on the border of North Sikkim district of Sikkim, India and Taplejung District of Nepal, while the other two are completely in Taplejung District. Nepal is home to the Kangchenjunga Conservation Area Project run by the World Wildlife Fund, in association with HMG in Nepal, the sanctuary is also home to the Red Panda and other snow animals, birds and plants. India's side of Kangchenjunga also has a protected park area called the Khangchendzonga National Park.

Although Kangchenjunga is the official spelling adopted by Douglas Freshfield, A.M. Kellas, and the Royal Geographical Society that gives the best indication of the Tibetan pronunciation, there are a number of alternative spellings which include Kangchen Dzö-nga, Khangchendzonga, Kanchenjanga, Kachendzonga, Kanchenjunga or Kangchanfanga. The final word on the use of the name Kangchenjunga came from His Highness Sir Tashi Namgyal, the Maharaja or chogyal of Sikkim, who stated that "although junga had no meaning in Tibetan, it really ought to have been Zod-nga (treasure, five) Kang-chen (snow, big) conveyed the meaning correctly". Following consultations with a Lieutenant-Colonel J.L.R. Weir (HMG political agent to Sikkim), he agreed that it was best to leave it as Kangchenjunga, and thus the name remained so by acceptance and usage. (from wiki)

© Ayan Khasnabis All Rights Reserved

Unauthorized use or reproduction for any reason is prohibited

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

Darjeeling is a City and a Municipality in the Indian state of West Bengal. It is located in the Mahabharat Range or Lesser Himalaya at an elevation of 2,164.1 m. It is noted for its tea industry and the Darjeeling Himalayan Railway, a UNESCO World Heritage Site. Darjeeling is the headquarters of Darjeeling district which has a partially autonomous status within the state of West Bengal. The development of the town dates back to the mid-19th century, when the colonial British administration set up a sanatorium and a military depot. Subsequently, extensive tea plantations were established in the region, and tea growers developed hybrids of black tea and created new fermentation techniques. The resultant distinctive Darjeeling tea is internationally recognized and ranks among the most popular of the black teas.

The Darjeeling Himalayan Railway connects the town with the plains and has one of the few steam locomotives still in service in India.

Darjeeling has several British-style public schools, which attract students from India and neighbouring countries. The varied culture of the town reflects its diverse demographic milieu consisting of Nepalis, Bhutia, Lepcha and other mainland Indian ethno-linguistic groups. Darjeeling, with its neighboring town of Kalimpong, was a center of the Gorkhaland movement (Separate State demand within India) in the 1980s. The town's fragile ecology has been threatened by a rising demand for environmental resources, stemming from growing tourist traffic and poorly planned urbanization.

HISTORY

The history of Darjeeling is intertwined with that of Sikkim, Nepal, British India and Bhutan. Until the early 19th century, the hilly area around Darjeeling was controlled by the kingdom of Sikkim, while the plains around Siliguri were intermittently occupied by the Kingdom of Nepal, with settlement consisting of a few villages of Lepcha and Kirati people. The Chogyal of Sikkim had been engaged in unsuccessful warfare against the Gorkhas of Nepal. From 1780, the Gorkhas made several attempts to capture the entire region of Darjeeling. By the beginning of 19th century, they had overrun Sikkim as far eastward as the Teesta River and had conquered and annexed the Terai. In the meantime, the British were engaged in preventing the Gorkhas from overrunning the whole of the northern frontier. The Anglo-Gorkha war broke out in 1814, which resulted in the defeat of the Gorkhas and subsequently led to the signing of the Sugauli Treaty in 1815. According to the treaty, Nepal had to cede all those territories which the Gorkhas had annexed from the Chogyal of Sikkim to the British East India Company (i.e. the area between Mechi River and Teesta River). Later in 1817, through the Treaty of Titalia, the British East India Company reinstated the Chogyal of Sikkim, restored all the tracts of land between the Mechi River and the Teesta River to the Chogyal of Sikkim and guaranteed his sovereignty.In 1828, a delegation of the British East India Company (BEIC) officials on its way to the Nepal-Sikkim border stayed in Darjeeling and decided that the region was a suitable site for a sanatorium for British soldiers. The company negotiated a lease of the area west of the Mahananda River from the Chogyal of Sikkim in 1835. In 1849, the BEIC director Arthur Campbell and the explorer and botanist Joseph Dalton Hooker were imprisoned in the region by the Sikkim Chogyal. The BEIC sent a force to free them. Continued friction between the BEIC and the Sikkim authorities resulted in the annexation of 1,700 km2 of territory by the British in 1850. In 1864, the Bhutanese rulers and the British signed the Treaty of Sinchula that ceded the passes leading through the hills and Kalimpong to the British. Further discord between Sikkim and the British resulted in a war, culminating in the signing of a treaty and the annexation by the British of the area east of the Teesta River in 1865. By 1866, Darjeeling district had assumed its current shape and size, covering an area of 3,200 km2.

During the British Raj, Darjeeling's temperate climate led to its development as a hill station for British residents seeking to escape the summer heat of the plains. The development of Darjeeling as a sanatorium and health resort proceeded briskly. Arthur Campbell, a surgeon with the Company, and Lieutenant Robert Napier were responsible for establishing a hill station there. Campbell's efforts to develop the station, attract immigrants to cultivate the slopes and stimulate trade resulted in a hundredfold increase in the population of Darjeeling between 1835 and 1849. The first road connecting the town with the plains was constructed between 1839 and 1842. In 1848, a military depot was set up for British soldiers, and the town became a municipality in 1850. Commercial cultivation of tea in the district began in 1856, and induced a number of British planters to settle there. Darjeeling became the formal summer capital of the Bengal Presidency after 1864. Scottish missionaries undertook the construction of schools and welfare centres for the British residents, laying the foundation for Darjeeling's notability as a centre of education. The opening of the Darjeeling Himalayan Railway in 1881 further hastened the development of the region. In 1899, Darjeeling was rocked by major landslides that caused severe damage to the town and the native population.

Under British rule, the Darjeeling area was initially a "Non-Regulation District", a scheme of administration applicable to economically less advanced districts in the British Raj; acts and regulations of the British Raj did not automatically apply to the district in line with rest of the country. In 1919, the area was declared a "backward tract". During the Indian independence movement, the Non-cooperation Movement spread through the tea estates of Darjeeling. There was also a failed assassination attempt by revolutionaries on Sir John Anderson, the Governor of Bengal in 1934. Subsequently, during the 1940s, Communist activists continued the nationalist movement against the British by mobilising the plantation workers and the peasants of the district.

Socio-economic problems of the region that had not been addressed during British rule continued to linger and were reflected in a representation made to the Constituent Assembly of India in 1947, which highlighted the issues of regional autonomy and Nepali nationality in Darjeeling and adjacent areas. After the independence of India in 1947, Darjeeling was merged with the state of West Bengal. A separate district of Darjeeling was established consisting of the hill towns of Darjeeling, Kurseong, Kalimpong and some parts of the Terai region. While the hill population comprised mainly ethnic Nepalis, the plains harboured a large ethnic Bengali population who were refugees from the Partition of India. A cautious and non-receptive response by the West Bengal government to most demands of the ethnic Nepali population led to increased calls, in the 1950s and 1960s, for Darjeeling's autonomy and for the recognition of the Nepali language; the state government acceded to the latter demand in 1961.

The creation of a new state of Sikkim in 1975, along with the reluctance of the Government of India to recognise Nepali as an official language under the Constitution of India, brought the issue of a separate state of Gorkhaland to the forefront. Agitation for a separate state continued through the 1980s, included violent protests during the 1986–88 period. The agitation ceased only after an agreement between the government and the Gorkha National Liberation Front (GNLF), resulting in the establishment of an elected body in 1988 called the Darjeeling Gorkha Hill Council (DGHC), which received autonomy to govern the district. Though Darjeeling became peaceful, the issue of a separate state lingered, fuelled in part by the lack of comprehensive economic development in the region even after the formation of the DGHC. New protests erupted in 2008–09, but both the Union and State governments rejected Gorkha Janmukti Morcha's (GJM) demand for a separate state. In July 2011, a pact was signed between GJM, the Government of West Bengal and the Government of India which includes the formation of a new autonomous, elected Gorkhaland Territorial Administration (GTA), a hill council endowed with more powers than its predecessor Darjeeling Gorkha Hill Council.

GEOGRAPHY

Darjeeling is the main town of the Sadar subdivision and also the headquarters of the district. It is located at an elevation of 2,200 m in the Darjeeling Himalayan hill region on the Darjeeling-Jalapahar range that originates in the south from Ghum. The range is Y-shaped with the base resting at Katapahar and Jalapahar and two arms diverging north of the Observatory Hill. The north-eastern arm dips suddenly and ends in the Lebong spur, while the north-western arm passes through North Point and ends in the valley near Tukver Tea Estate. The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Kanchenjunga, the world's third-highest peak, 8,598 m high, is the most prominent mountain visible. In days clear of clouds, Nepal's Mount Everest, 8,850 m high, can be seen. The hills of Darjeeling are part of the Mahabharat Range or Lesser Himalaya. The soil is chiefly composed of sandstone and conglomerate formations, which are the solidified and upheaved detritus of the great range of Himalaya. However, the soil is often poorly consolidated (the permeable sediments of the region do not retain water between rains) and is not considered suitable for agriculture. The area has steep slopes and loose topsoil, leading to frequent landslides during the monsoons. According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.

FLORA AND FAUNA

Darjeeling is a part of the Eastern Himalayan zoo-geographic zone. Flora around Darjeeling comprises sal, oak, semi-evergreen, temperate and alpine forests. Dense evergreen forests of sal and oak lie around the town, where a wide variety of rare orchids are found. The Lloyd's Botanical Garden preserves common and rare species of plants, while the Padmaja Naidu Himalayan Zoological Park specialises in conserving and breeding endangered Himalayan species. The town of Darjeeling and surrounding region face deforestation due to increasing demand for wood fuel and timber, as well as air pollution from increasing vehicular traffic.Wildlife in the district is protected by the wildlife wing of the West Bengal Forest Department. The fauna found in Darjeeling includes several species of ducks, teals, plovers and gulls that pass Darjeeling while migrating to and from Tibet. Small mammals found in the region include civets, mongooses and badgers. The nearby Jaldapara National Park consists of semi-evergreen and sal forests. Animals found here include the one-horned rhinoceros, elephant, tiger, leopard and hog deer, while the main bird species include the Bengal florican and herons. As of 2009, work was in progress for setting up a conservation centre for red pandas in Darjeeling.

CLIMATE

Darjeeling has a temperate climate (Köppen: Cwb, subtropical highland climate) with wet summers caused by monsoon rains. The annual mean maximum temperature is 15.98 °C while the mean minimum temperature is 8.9 °C, with monthly mean temperatures range from 5 to 17 °C. The lowest temperature recorded was −24 °C on 11 February 1905. The average annual precipitation is 309.2 cm, with an average of 126 days of rain in a year. The highest rainfall occurs in July. The heavy and concentrated rainfall that is experienced in the region, aggravated by deforestation and haphazard planning, often causes devastating landslides, leading to loss of life and property.

CIVIC ADMINISTRATION

The Darjeeling urban agglomeration consists of Darjeeling Municipality and the Pattabong Tea Garden.Established in 1850, the Darjeeling municipality maintains the civic administration of the town, covering an area of 10.57 km2. The municipality consists of a board of councillors elected from each of the 32 wards of Darjeeling town as well as a few members nominated by the state government. The board of councillors elects a chairman from among its elected members; the chairman is the executive head of the municipality. The Gorkha Janmukti Morcha (GJMM) holds power in the municipality As of 2011.From 1988 to 2012, the Gorkha-dominated hill areas of Darjeeling district was under the jurisdiction of the Darjeeling Gorkha Hill Council (DGHC). In 2012, the DGHC was replaced by the Gorkhaland Territorial Administration (GTA). The elected members of this body are authorised to manage certain affairs of the hills, including education, health and tourism. Law and order in Darjeeling town comes under the jurisdiction of the district police force, which is a part of the West Bengal Police; a Deputy Superintendent of Police oversees the town's security and law affairs. Darjeeling municipality area has two police stations at Darjeeling and Jorebungalow.

UTILITIES

Natural springs in the Senchal Range provide most of Darjeeling's water supply. Water collected is routed through stone conduits to two lakes that were constructed in 1910 and 1932, from where it is piped to the town after purification at the Jorebungalow filtration plant. During the dry season, when water supplied by springs is insufficient, water is pumped from Khong Khola, a nearby small perennial stream. There is a steadily widening gap between water supply and demand; just over 50% of the town's households are connected to the municipal water supply system. Various efforts made to augment the water supply, including the construction of a third storage reservoir in 1984, have failed to yield desired results. The town has an underground sewage system, covering about 40% of the town area, that collects domestic waste and conveys it to septic tanks for disposal. Solid waste is disposed of in a nearby dumping ground, which also houses the town's crematorium. Doorstep collection of garbage and segregation of biodegradable and non-biodegradable waste have been implemented since 2003. Vermicomposting of vegetable waste is carried out with the help of non-governmental organisations. In June 2009, in order to reduce waste, the municipality proposed the ban of plastic carry bags and sachets in the town.

Darjeeling got from 1897 up to the early 1990s hydroelectricity from the nearby Sidrapong Hydel Power Station, such being the first town in India supplied with hydropower. Today, electricity is supplied by the West Bengal State Electricity Board from other places. The town often suffers from power outages and the electrical supply voltage is unstable, making voltage stabilisers popular with many households. Almost all of the primary schools are now maintained by Darjeeling Gorkha Autonomous Hill Council. The total length of all types of roads within the municipal area is around 134 km. The West Bengal Fire Service provides emergency services for the town.

ECONOMY

The two most significant contributors to Darjeeling's economy are tourism and the tea industry. Darjeeling tea, due to the unique agro-climatic conditions of Darjeeling, has a distinctive natural flavour, is internationally reputed and recognised as a geographical indicator. Darjeeling produces 7% of India's tea output, approximately 9,000,000 kilograms every year. The tea industry has faced competition in recent years from tea produced in other parts of India as well as other countries like Nepal. Widespread concerns about labour disputes, worker layoffs and closing of estates have affected investment and production. Several tea estates are being run on a workers' cooperative model, while others are being planned for conversion into tourist resorts. More than 60% of workers in the tea gardens are women. Besides tea, the most widely cultivated crops include maize, millets, paddy, cardamom, potato and ginger. Darjeeling had become an important tourist destination as early as 1860. It is reported to be the only location in eastern India that witnesses large numbers of foreign tourists. It is also a popular filming destination for Bollywood and Bengali cinema. Satyajit Ray shot his film Kanchenjungha (1962) here, and his Feluda series story, Darjeeling Jomjomaat was also set in the town. Bollywood movies Aradhana (1969), Main Hoon Na (2004), and more recently Barfi! (2012) have been filmed here. Tourist inflow into Darjeeling has been affected by the political instability in the region, and agitations in the 1980s and 2000s have hit the tourism industry hard.

TRANSPORT

Darjeeling can be reached by the 88 km long Darjeeling Himalayan Railway from New Jalpaiguri, or by National Highway 55, from Siliguri, 77 km away.The Darjeeling Himalayan Railway is a 600 mm narrow-gauge railway that was declared a World Heritage Site by UNESCO in 1999 for being "an outstanding example of the influence of an innovative transportation system on the social and economic development of a multi-cultural region, which was to serve as a model for similar developments in many parts of the world", becoming only the second railway in the world to have this honour.Bus services and hired vehicles connect Darjeeling with Siliguri and Darjeeling has road connections with Bagdogra, Gangtok and Kathmandu and the neighbouring towns of Kurseong and Kalimpong. However, road and railway communications often get disrupted in the monsoons because of landslides. The nearest airport is Bagdogra Airport, located 90 km from Darjeeling. Within the town, people usually traverse by walking. Residents also use two-wheelers and hired taxis for travelling short distances. The Darjeeling Ropeway, functional since 1968, was closed in 2003 after an accident killed four tourists. It was proposed to be reopened in 2007, and finally opened in February 2012.

DEMOGRAPHICS

According to provisional results of 2011 census of India, Darjeeling urban agglomeration has a population of 132,016, out of which 65,839 were males and 66,177 were females. The sex ratio is 1005 females per 1,000 males. The 0–6 years population is 7,382. Effective literacy rate for the population older than 6 years is 93.17 per cent. According to the 2001 census, the Darjeeling urban agglomeration, with an area of 12.77 km2 had a population of 109,163, while the municipal area had a population of 107,530. The population density of the municipal area was 10,173 per km2. The sex ratio was 1,017 females per 1,000 males, which was higher than the national average of 933 females per 1000 males. The three largest religions were Hinduism, Buddhism and Christianity, in that order. The majority of the populace are Gorkhas of ethnic Nepali background. Indigenous ethnic groups include the Limbu, Rai, Magars, Gurung, Tamangs, Lepchas, Bhutias, Sherpas and Newars. Other communities that inhabit Darjeeling include the Marwaris, Anglo-Indians, Chinese, Biharis, Tibetans and Bengali. The most commonly spoken languages are Nepali, Hindi, Bengali and English. Darjeeling has seen a significant growth in its population, its decadal growth rate being 47% between 1991 and 2001. The colonial town had been designed for a population of only 10,000, and subsequent growth has created extensive infrastructural and environmental problems. The district's forests and other natural wealth have been adversely affected by an ever-growing population. Environmental degradation, including denudation of the surrounding hills has adversely affected Darjeeling's appeal as a tourist destination. The official language of West Bengal is Bengali, additional official languages in Darjeeling are English and Nepali.

CULTURE

Apart from the major religious festivals of Dashain (Durga puja), Tihar (Diwali) and Christmas the diverse ethnic populace of the town celebrates several local festivals. The Lepchas and Bhutias celebrate new year in January, while Tibetans celebrate their new year, Losar, in February–March. The birthday of the Buddha is celebrated in mid-June with processions. Darjeeling Carnival, initiated by a civil society movement known as The Darjeeling Initiative, is a ten-day carnival held every year during the winter with portrayal of the Darjeeling Hill's musical and cultural heritage as its central theme. A popular food in Darjeeling is the Nepalese and Tibetan momo, a steamed dumpling containing meat cooked in a doughy wrapping and served with clear soup and achar. A form of Tibetan noodle called thukpa, served in soup form is also popular. Other commonly eaten dishes include alu dum, a potato preparation, and shaphalay, Tibetan bread stuffed with meat. Fermented foods and beverages are consumed by a large percentage of the population. Fermented foods include preparations of soybean, bamboo shoots, milk and Sel roti, which is made from rice. Tea is the most popular beverage, the Tibetan version is also drunk.Alcoholic beverages include Tongba, Jnaard and Chhaang, variations of a local beer made from fermenting finger millet.

Colonial architecture characterises many buildings in Darjeeling, exemplified by several mock Tudor residences, Gothic churches, the Raj Bhawan, Planters' Club and various educational institutions. Buddhist monasteries showcase the pagoda style architecture. Darjeeling is regarded as a centre of music and a niche for musicians and music admirers. Singing and playing musical instruments is a common pastime among the resident population, who take pride in the traditions and role of music in cultural life. Darjeeling also has a Peace Pagoda built in 1992 by the Japanese Buddhist organisation Nipponzan Myohoji.

EDUCATION

There are 52 primary schools, 21 high schools and 4 colleges in the town. Darjeeling's schools are either run by the state government or by private and religious organisations. Schools mainly use English and Nepali as their media of instruction, although there is the option to learn the national language Hindi and the official state language Bengali. The schools are either affiliated with the ICSE, the CBSE, or the West Bengal Board of Secondary Education. Having been a summer retreat for the British in India, Darjeeling became the place of choice for the establishment of public schools on the model of Eton, Harrow and Rugby, allowing the children of British officials to obtain an exclusive education. Institutions such as Mount Hermon School, St. Robert's H.S. School, St. Joseph's College (School Dept.), Loreto Convent, and St. Paul's School are renowned as centres of educational excellence. Darjeeling has four colleges - St. Joseph's College, Southfield College (earlier known as Loreto College), Darjeeling Government College and Sri Ramakrishna B.T. College - all affiliated to the University of North Bengal in Siliguri.

TOURIST ATTRACTIONS

Tiger Hill is located in Darjeeling, in the Indian State of West Bengal, and is the summit of Ghoom, the highest railway station in the Darjeeling Himalayan Railway - a UNESCO World Heritage Site.

Padmaja Naidu Himalayan Zoological Park is a 67.56-acre zoo in the town of Darjeeling in the Indian state of West Bengal. The zoo was opened in 1958, and an average elevation of 7,000 feet, is the largest high altitude zoo in India.

The Darjeeling Himalayan Railway, also known as the "Toy Train", is a 2 ft (610 mm) narrow gauge railway that runs between New Jalpaiguri and Darjeeling in the Indian state of West Bengal, India.

The Batasia Loop is a spiral railway created to lower the gradient of ascent of the Darjeeling Himalayan Railway in Darjeeling district of West Bengal, India. At this point, the track spirals around over itself through a tunnel and over a hilltop.

Peace Pagoda, Darjeeling or Darjeeling Peace Pagoda is one of the Peace Pagodas designed to provide a focus for people of all races and creeds to help unite them in their search for world peace.

Windamere Hotel, built in the 1930s, is a heritage hotel situated on Observatory Hill, in Darjeeling, India.

Mirik is a picturesque tourist spot nestled in the serene hills of Darjeeling district in West Bengal, India. The name Mirik comes from the Lepcha words Mir-Yok meaning "place burnt by fire".

Samsing is a small hill village and tourist spot in the Malbazar subdivision of Jalpaiguri district of West Bengal situated at an elevation of 3000 ft in the foothills of Jalpaiguri and Darjeeling districts border.

Suntalekhola or Suntaley Khola is a small village and a tourist spot in the Darjeeling District of West Bengal. The altitude of the place ranges from 650 to 950 m. It gets it name from a small stream: Suntaley Khola.

Bhutia Busty monastery or Karmaa Dorjee Chyoling monastery is a Buddhist monastery located in Tongsong, Darjeeling, India. It belongs to the Red Sect of Buddhist Lamas.

DARJEELING CARNIVAL

Darjeeling Carnival is a ten-day carnival arranged in the town of Darjeeling, West Bengal, India.The carnival consists of several functions like poetry-reading sessions, painting and photo exhibitions, tea-drinking ceremonies, a Land Rover rally, music concerts and ethnic food festivals.

WIKIPEDIA

The Himalayas or Himalaya (/ˌhɪməˈleɪ.ə/ or /hɪˈmɑːləjə/) is a mountain range in the Indian subcontinent, which separates the Indo-Gangetic Plain from the Tibetan Plateau. Geopolitically, it covers the Himalayan states and regions. This range is home to nine of the ten highest peaks on Earth, including the highest above sea level, Mount Everest. The Himalayas have profoundly shaped the cultures of South Asia. Many Himalayan peaks are sacred in Dharmic religions such as Hinduism and Buddhism.

The Himalayas are bordered on the north by the Tibetan Plateau, on the south by the Indo-Gangetic Plain, on the northwest by the Karakoram and Hindu Kush ranges and on the east by the Indian states of Sikkim, the Darjeeling district of West Bengal, Assam, Arunachal Pradesh and Manipur. The Hindu Kush, Karakoram and Himalayas together form the "Hindu Kush Himalayan Region" (HKH). The western anchor of the Himalayas, Nanga Parbat, lies just south of the northernmost bend of the Indus River; the eastern anchor, Namcha Barwa, is just west of the great bend of the Yarlung Tsangpo River. The Himalayas span five countries: Nepal, India, Bhutan, China (Tibet), and Pakistan, the first three countries having sovereignty over most of the range.

Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre-long arc. The range varies in width from 400 kilometres in the west to 150 kilometres in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000–3000 m, known as the Lower Himalayan Range.

Three of the world's major rivers (the Indus, the Ganges and the Brahmaputra) arise in the Himalayas. While the Indus and the Brahmaputra rise near Mount Kailash in Tibet, the Ganges rises in the Indian state of Uttarakhand. Their combined drainage basin is home to some 600 million people.

ETYMOLOGY

The name Himālaya is from Sanskrit: hima (snow) + ālaya (dwelling), and literally means "abode of snow"

ECOLOGY

The flora and fauna of the Himalayas vary with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the southern front of the range. This diversity of altitude, rainfall and soil conditions combined with the very high snow line supports a variety of distinct plant and animal communities. The extremes of high altitude (low atmospheric pressure) combined with extreme cold favor extremophile organisms.

The unique floral and faunal wealth of the Himalayas is undergoing structural and compositional changes due to climate change. The increase in temperature is shifting various species to higher elevations. The oak forest is being invaded by pine forests in the Garhwal Himalayan region. There are reports of early flowering and fruiting in some tree species, especially rhododendron, apple and box myrtle. The highest known tree species in the Himalayas is Juniperus tibetica located at 4,900 metres in Southeastern Tibet.

GEOLOGY

The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

During the Upper Cretaceous, about 70 million years ago, the north-moving Indo-Australian plate (which has subsequently broken into the Indian Plate and the Australian plate) was moving at about 15 cm per year. About 50 million years ago this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor, and the volcanoes that fringed its edges. Since both plates were composed of low density continental crust, they were thrust faulted and folded into mountain ranges rather than subducting into the mantle along an oceanic trench. An often-cited fact used to illustrate this process is that the summit of Mount Everest is made of marine limestone from this ancient ocean.

Today, the Indian plate continues to be driven horizontally below the Tibetan Plateau, which forces the plateau to continue to move upwards. The Indian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

During the last ice age, there was a connected ice stream of glaciers between Kangchenjunga in the east and Nanga Parbat in the west. In the west, the glaciers joined with the ice stream network in the Karakoram, and in the north, joined with the former Tibetan inland ice. To the south, outflow glaciers came to an end below an elevation of 1,000–2,000 metres. While the current valley glaciers of the Himalaya reach at most 20 to 32 kilometres in length, several of the main valley glaciers were 60 to 112 kilometres long during the ice age. The glacier snowline (the altitude where accumulation and ablation of a glacier are balanced) was about 1,400–1,660 metres lower than it is today. Thus, the climate was at least 7.0 to 8.3 °C colder than it is today.

HYDROLOGY

The Himalayas contain the third-largest deposit of ice and snow in the world, after Antarctica and the Arctic. The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km3 of fresh water. Its glaciers include the Gangotri and Yamunotri (Uttarakhand) and Khumbu glaciers (Mount Everest region), Langtang glacier (Langtang region) and Zemu (Sikkim).

Owing to the mountains' latitude near the Tropic of Cancer, the permanent snow line is among the highest in the world at typically around 5,500 metres. In contrast, equatorial mountains in New Guinea, the Rwenzoris and Colombia have a snow line some 900 metres lower. The higher regions of the Himalayas are snowbound throughout the year, in spite of their proximity to the tropics, and they form the sources of several large perennial rivers, most of which combine into two large river systems:

- The western rivers, of which the Indus is the largest, combine into the Indus Basin. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through India and then through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

- Most of the other Himalayan rivers drain the Ganges-Brahmaputra Basin. Its main rivers are the Ganges, the Brahmaputra and the Yamuna, as well as other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganges and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta, the Sunderbans.

The easternmost Himalayan rivers feed the Irrawaddy River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, Yangtze and Huang He (Yellow River) all originate from parts of the Tibetan Plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years, scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. For example, glacial lakes have been forming rapidly on the surface of debris-covered glaciers in the Bhutan Himalaya during the last few decades. Although the effect of this will not be known for many years, it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers during the dry seasons.

LAKES

The Himalayan region is dotted with hundreds of lakes. Most lakes are found at altitudes of less than 5,000 m, with the size of the lakes diminishing with altitude. Tilicho Lake in Nepal in the Annapurna massif is one of the highest lakes in the world. Pangong Tso, which is spread across the border between India and China, and Yamdrok Tso, located in central Tibet, are amongst the largest with surface areas of 700 km², and 638 km², respectively. Other notable lakes include She-Phoksundo Lake in the Shey Phoksundo National Park of Nepal, Gurudongmar Lake, in North Sikkim, Gokyo Lakes in Solukhumbu district of Nepal and Lake Tsongmo, near the Indo-China border in Sikkim.

Some of the lakes present a danger of a glacial lake outburst flood. The Tsho Rolpa glacier lake in the Rowaling Valley, in the Dolakha District of Nepal, is rated as the most dangerous. The lake, which is located at an altitude of 4,580 metres has grown considerably over the last 50 years due to glacial melting.

The mountain lakes are known to geographers as tarns if they are caused by glacial activity. Tarns are found mostly in the upper reaches of the Himalaya, above 5,500 metres.

IMPACT ON CLIMATE

The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.

RELIGIOUS OF THE REGION

In Hinduism, the Himalayas have been personified as the god Himavat, father of Ganga and Parvati.

Several places in the Himalayas are of religious significance in Buddhism, Hinduism, Jainism and Sikhism. A notable example of a religious site is Paro Taktsang, where Padmasambhava is said to have founded Buddhism in Bhutan. Padmasambhava is also worshipped as the patron saint of Sikkim.

A number of Vajrayana Buddhist sites are situated in the Himalayas, in Tibet, Bhutan and in the Indian regions of Ladakh, Sikkim, Arunachal Pradesh, Spiti and Darjeeling. There were over 6,000 monasteries in Tibet, including the residence of the Dalai Lama. Bhutan, Sikkim and Ladakh are also dotted with numerous monasteries. The Tibetan Muslims have their own mosques in Lhasa and Shigatse.

RESOURCES

The Himalayas are home to a diversity of medicinal resources. Plants from the forests have been used for millennia to treat conditions ranging from simple coughs to snake bites. Different parts of the plants - root, flower, stem, leaves, and bark - are used as remedies for different ailments. For example, a bark extract from an abies pindrow tree is used to treat coughs and bronchitis. Leaf and stem paste from an arachne cordifolia is used for wounds and as an antidote for snake bites. The bark of a callicarpa arborea is used for skin ailments. Nearly a fifth of the gymnosperms, angiosperms, and pteridophytes in the Himalayas are found to have medicinal properties, and more are likely to be discovered.

Most of the population in some Asian and African countries depend on medicinal plants rather than prescriptions and such (Gupta and Sharma, vii). Since so many people use medicinal plants as their only source of healing in the Himalayas, the plants are an important source of income. This contributes to economic and modern industrial development both inside and outside the region (Gupta and Sharma, 5). The only problem is that locals are rapidly clearing the forests on the Himalayas for wood, often illegally (Earth Island Journal, 2). This means that the number of medicinal plants is declining and that some of them might become rarer or, in some cases, go extinct.

Although locals are clearing out portions of the forests in the Himalayas, there is still a large amount of greenery ranging from the tropical forests to the Alpine forests. These forests provide wood for fuel and other raw materials for use by industries. There are also many pastures for animals to graze upon (Mohita, sec. Forest and Wealth). The many varieties of animals that live in these mountains do so based on the elevation. For example, elephants and rhinoceros live in the lower elevations of the Himalayas, also called the Terai region. Also, found in these mountains are the Kashmiri stag, black bears, musk deer, langur, and snow leopards. The Tibetan yak are also found on these mountains and are often used by the people for transportation. However, the populations of many of these animals and still others are declining and are on the verge of going extinct (Admin, sec. Flora and Fauna).

The Himalayas are also a source of many minerals and precious stones. Amongst the tertiary rocks, are vast potentials of mineral oil. There is coal located in Kashmir, and precious stones located in the Himalayas. There is also gold, silver, copper, zinc, and many other such minerals and metals located in at least 100 different places in these mountains (Mohita, sec. Minerals).

CULTURE

There are many cultural aspects of the Himalayas. For the Hindus, the Himalayas are personified as Himavath, the father of the goddess Parvati (Gupta and Sharma, 4). The Himalayas is also considered to be the father of the river Ganges. The Mountain Kailash is a sacred peak to the Hindus and is where the Lord Shiva is believed to live (Admin, sec. Centre of Religion). Two of the most sacred places of pilgrimage for the Hindus is the temple complex in Pashupatinath and Muktinath, also known as Saligrama because of the presence of the sacred black rocks called saligrams (Zurick, Julsun, Basanta, and Birendra, 153).

The Buddhists also lay a great deal of importance on the mountains of the Himalayas. Paro Taktsang is the holy place where Buddhism started in Bhutan (Admin, sec. Centre of Religion). The Muktinath is also a place of pilgrimage for the Tibetan Buddhists. They believe that the trees in the poplar grove came from the walking sticks of eighty-four ancient Indian Buddhist magicians or mahasiddhas. They consider the saligrams to be representatives of the Tibetan serpent deity known as Gawo Jagpa (Zurick, Julsun, Basanta, and Birendra, 153).

The Himalayan people’s diversity shows in many different ways. It shows through their architecture, their languages and dialects, their beliefs and rituals, as well as their clothing (Zurick, Julsun, Basanta, and Birendra, 78). The shapes and materials of the people’s homes reflect their practical needs and the beliefs. Another example of the diversity amongst the Himalayan peoples is that handwoven textiles display unique colors and patterns that coincide with their ethnic backgrounds. Finally, some people place a great importance on jewelry. The Rai and Limbu women wear big gold earrings and nose rings to show their wealth through their jewelry (Zurick, Julsun, Basanta, and Birendra, 79).

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