++++++++ FROM WIKIPEDIA ++++++++++

 

Kalimpong is a hill station in the Indian state of West Bengal. It is located at an average elevation of 1,250 metres (4,101 ft). The town is the headquarters of the Kalimpong district.The Indian Army's 27 Mountain Division is located on the outskirts of the town.

 

Kalimpong is known for its educational institutions, many of which were established during the British colonial period.[5] It used to be a gateway in the trade between Tibet and India before China's annexation of Tibet and the Sino-Indian War. Kalimpong and neighbouring Darjeeling were major centres calling for a separate Gorkhaland state in the 1980s, and more recently in 2010.

 

The municipality sits on a ridge overlooking the Teesta River and is a tourist destination owing to its temperate climate, magnificent Himalayan beauty and proximity to popular tourist locations in the region. Horticulture is important to Kalimpong: It has a flower market notable for its wide array of orchids; nurseries, which export Himalayan grown flower bulbs, tubers and rhizomes, contribute to the economy of Kalimpong.[2] Home to Nepalisindigenous Lepchas, other ethnic groups and non-native immigrants from other parts of India, the town is a religious centre of Buddhism. The Tibetan Buddhist monastery Zang Dhok Palri Phodang holds a number of rare Tibetan Buddhist scriptures.[6]

 

The Kalimpong Science Centre, established under the Darjeeling Gorkha Hill Council (DGHC) in 2008 is a recent addition to its many tourist attractions. The Science Centre, which provides for scientific awareness among the students of the town and the locals sits atop the Deolo Hill.

 

Name origin

The precise etymology of the name Kalimpong remains unclear. There are many theories on the origin of the name. One widely accepted theory claims that the name "Kalimpong" means "Assembly (or Stockade) of the King's Ministers" in Tibetan, derived from kalon ("King's ministers") and pong ("stockade"). It may be derived from the translation "ridge where we play" from Lepcha, as it was known to be the place for traditional tribal gatherings for summer sporting events. People from the hills call the area Kalempung ("the black spurs").[7]

 

According to K.P. Tamsang, author of The Untold and Unknown Reality about the Lepchas, the term Kalimpong is deduced from the name Kalenpung, which in Lepcha means "Hillock of Assemblage";[8] in time, the name was distorted to Kalebung, and later further contorted to Kalimpong. Another possible derivation points to Kaulim, a fibrous plant found in abundance in the region.[9]

History

Katherine Graham Memorial Chapel, Dr. Graham's Homes

The Clock Tower of Kalimpong.

 

Until the mid-19th century, the area around Kalimpong was ruled in succession by the Sikkimese and Bhutanese kingdoms.[8][10] Under Sikkimese rule, the area was known as Dalingkot.[11] In 1706, the king of Bhutan won this territory from the Sikkimese monarch and renamed it Kalimpong.[11] Overlooking the Teesta Valley, Kalimpong is believed to have once been the forward position of the Bhutanese in the 18th century. The area was sparsely populated by the indigenous Lepcha community and migrant Bhutia and Limbu tribes.

 

After the Anglo-Bhutan War in 1864, the Treaty of Sinchula (1865) was signed, in which Bhutanese held territory east of the Teesta River was ceded to the British East India Company.[8] At that time, Kalimpong was a hamlet, with only two or three families known to reside there.[12] The first recorded mention of the town was a fleeting reference made that year by Ashley Eden, a government official with the Bengal Civil Service. Kalimpong was added to district of Darjeeling in 1866. In 1866–1867 an Anglo-Bhutanese commission demarcated the common boundaries between the two, thereby giving shape to the Kalimpong subdivision and the Darjeeling district.[13]

 

After the war, the region became a subdivision of the Western Duars district, and the following year it was merged with the district of Darjeeling.[8] The temperate climate prompted the British to develop the town as an alternative hill station to Darjeeling, to escape the scorching summer heat in the plains. Kalimpong's proximity to the Nathu La and Jelep La passes (La means "pass"), offshoots of the ancient Silk Road, was an added advantage. It soon became an important trading outpost in the trade of furs, wools and food grains between India and Tibet.[14] The increase in commerce attracted large numbers of Nepali's from the neighbouring Nepal and the lower regions of Sikkim, the areas where, Nepali's were residing since the Gorkha invasion of Sikkim in 1790. The movement of people into the area, transformed Kalimpong from a small hamlet with a few houses, to a thriving town with increased economic prosperity. Britain assigned a plot within Kalimpong to the influential Bhutanese Dorji family, through which trade and relations with Bhutan flowed. This later became Bhutan House, a Bhutanese administrative and cultural centre.[15][16][17]

 

The arrival of Scottish missionaries saw the construction of schools and welfare centres for the British.[12] Rev. W. Macfarlane in the early 1870s established the first schools in the area.[12] The Scottish University Mission Institution was opened in 1886, followed by the Kalimpong Girls High School. In 1900, Reverend J.A. Graham founded the Dr. Graham's Homes for destitute Anglo-Indian students.[12] The young missionary (and aspiring writer and poet) Aeneas Francon Williams, aged 24, arrived in Kalimpong in 1910 to take up the post of assistant schoolmaster at Dr. Graham's Homes,[18] where he later became Bursar and remained working at the school for the next fourteen years.[19] From 1907 onwards, most schools in Kalimpong had started offering education to Indian students. By 1911, the population comprised many ethnic groups, including Nepalis, Lepchas, Tibetans, Muslims, the Anglo-Indian communities. Hence by 1911, the population had swollen to 7,880.[12]

 

Following Indian independence in 1947, Kalimpong became part of the state of West Bengal, after Bengal was partitioned between India and East Pakistan. With China's annexation of Tibet in 1959, many Buddhist monks fled Tibet and established monasteries in Kalimpong. These monks brought many rare Buddhist scriptures with them. In 1962, the permanent closure of the Jelep Pass after the Sino-Indian War disrupted trade between Tibet and India, and led to a slowdown in Kalimpong's economy. In 1976, the visiting Dalai Lama consecrated the Zang Dhok Palri Phodang monastery, which houses many of the scriptures.[12]

Most large houses in Kalimpong were built during the British era. In the background is Mount Kangchenjunga.

Morgan House is a classic example of colonial architecture in Kalimpong.

 

Between 1986 and 1988, the demand for a separate state of Gorkhaland and Kamtapur based on ethnic lines grew strong. Riots between the Gorkha National Liberation Front (GNLF) and the West Bengal government reached a stand-off after a forty-day strike. The town was virtually under siege, and the state government called in the Indian army to maintain law and order. This led to the formation of the Darjeeling Gorkha Hill Council, a body that was given semi-autonomous powers to govern the Darjeeling district, except the area under the Siliguri subdivision. Since 2007, the demand for a separate Gorkhaland state has been revived by the Gorkha Janmukti Morcha and its supporters in the Darjeeling hills.[20] The Kamtapur People's Party and its supporters' movement for a separate Kamtapur state covering North Bengal have gained momentum.[21]

Geography

A view from the Deolo Resort, atop Deolo Hill, Kalimpong's highest point

 

The town centre is on a ridge connecting two hills, Deolo Hill and Durpin Hill,[12] at an elevation of 1,247 m (4,091 ft). Deolo, the highest point in Kalimpong, has an altitude of 1,704 m (5,591 ft) and Durpin Hill is at an elevation of 1,372 m (4,501 ft). The River Teesta flows in the valley below and separates Kalimpong from the state of Sikkim. The soil in the Kalimpong area is typically reddish in color. Occasional dark soils are found due to extensive existence of phyllite and schists.[22] The Shiwalik Hills, like most of the Himalayan foothills, have steep slopes and soft, loose topsoil, leading to frequent landslides in the monsoon season.[22] The hills are nestled within higher peaks and the snow-clad Himalayan ranges tower over the town in the distance. Mount Kanchenjunga at 8,586 m (28,169 ft) the world's third tallest peak,[23] is clearly visible from Kalimpong.[2]

View of the Himalaya range

 

Kalimpong has five distinct seasons: spring, summer, autumn, winter and the monsoons. The annual temperature ranges from a high of 30 °C (86 °F) to a low of 9 °C (48 °F). Summers are mild, with an average maximum temperature of 30 °C (86 °F) in August.[24] Summers are followed by the monsoon rains which lash the town between June and September. The monsoons are severe, often causing landslides which sequester the town from the rest of India. Winter lasts from December to February, with the maximum temperature being around 15 °C (59 °F). During the monsoon and winter seasons, Kalimpong is often enveloped by fog.[25]

Economy

Oranges grown in the hillsides are exported to many parts of India.

 

Tourism is the most significant contributor to Kalimpong's economy.[26] The summer and spring seasons are the most popular with tourists, keeping many of town's residents employed directly and indirectly. The town—earlier an important trade post between India and Tibet—hopes to boost its economy after the reopening of the Nathu La (pass) in April 2006.[27] Though this has resumed Indo–China border trades,[28] it is expected that Kalimpong will have a better chance of revival as a hub for Indo–China trades if the demand of local leaders for reopening of Jelep La pass also is met.[28]

 

Kalimpong is a major ginger growing area of India. Kalimpong and the state of Sikkim together contribute 15 percent of ginger produced in India.[29] The Darjeeling Himalayan hill region is internationally famous for its tea industry.[30] However, most of the tea gardens are on the western side of Teesta river (towards the town of Darjeeling) and so tea gardens near Kalimpong contribute only 4 percent of total tea production of the region. In Kalimpong division, 90 percent of land is cultivable but only 10 percent is used for tea production.[31] Kalimpong is well known for its flower export industry—especially for its wide array of indigenous orchids and gladioli.[32]

 

A significant contributor to the town's economy is education sector.[26] The schools of Kalimpong, besides imparting education to the locals, attract a significant number of students from the plains, the neighbouring state of Sikkim and countries such as Bhutan, Bangladesh, Nepal and Thailand.[26]

 

Many establishments cater to the Indian army bases near the town, providing it with essential supplies. Small contributions to the economy come by the way of the sale of traditional arts and crafts of Sikkim and Tibet. Government efforts related to sericulture, seismology, and fisheries provide a steady source of employment to many of its residents.

 

Kalimpong is well renowned for its cheese, noodles and lollipops. Kalimpong exports a wide range of traditional handicrafts, wood-carvings, embroidered items, bags and purses with tapestry work, copper ware, scrolls, Tibetan jewellery and artifacts.[32][33]

Transport

NH31A winds along the banks of the river Teesta near Kalimpong.

 

Kalimpong is located off the National Highway 31A (NH31A), which links Sevok to Gangtok. The NH31A is an offshoot of the NH 31, which connects Sevok to Siliguri.[34] These two National Highways together, via Sevok, links Kalimpong to the plains.[35] Regular bus services and hired vehicles connect Kalimpong with Siliguri and the neighbouring towns of Kurseong, Darjeeling and Gangtok. Four wheel drives are popular means of transport, as they can easily navigate the steep slopes in the region. However, road communication often get disrupted in the monsoons due to landslides. In the town, people usually travel by foot. Residents also use bicycle, two-wheelers and hired taxis for short distances.

 

The nearest airport is in Bagdogra near Siliguri, about 80 kilometres (50 mi) from Kalimpong. Air India, Jet Airways and Druk Air (Bhutan) are the four major carriers that connect the airport to Delhi, Kolkata, Paro (Bhutan), Guwahati and Bangkok (Thailand). The closest major railway station is New Jalpaiguri, on the outskirts of Siliguri,[2] which is connected with almost all major cities of the country.

Demographics

Population growth

 

At the 2011 India census,[37] Kalimpong town area had a population of 42,988, of which 52% were male and 48% female.[37]

 

At the 2001 census,[38] Kalimpong had an average literacy rate of 79%, higher than the national average of 59.5%: male literacy was 84%, and female literacy was 73%. In Kalimpong, 8% of the population was under 6 years of age. The Scheduled castes and scheduled tribes population for Kalimpong was 5,100 and 5,121 respectively.[39]

Civic administration

 

Kalimpong is the headquarters of the Kalimpong district. The semi-autonomous Darjeeling Gorkha Hill Council (DGHC), set up by the West Bengal government in 1988, administers this district as well as the Darjeeling Sadar and Kurseong subdivisions.[40] Kalimpong elects eight councillors to the DGHC, who manages the departments of Public Health, Education, Public Works, Transport, Tourism, Market, Small scale industries, Agriculture, Agricultural waterways, Forest (except reserved forests), Water, Livestock, Vocational Training and Sports and Youth services.[41] The district administration of Darjeeling, which is the authoritative body for the departments of election, panchayat, law and order, revenue, etc., also acts as an interface of communication between the Council and the State Government.[41] The rural area in the district covers three community development blocks Kalimpong I, Kalimpong II and Gorubathan consisting of forty-two gram panchayats.[42] A Sub-Divisional Officer (SDO) presides over the Kalimpong subdivision. Kalimpong has a police station that serves the municipality and 18 gram panchayats of Kalimpong–I CD block.[43]

 

The Kalimpong municipality, which was established in 1945,[39] is in charge of the infrastructure of the town such as potable water and roads. The municipal area is divided into twenty-three wards.[44] Kalimpong municipality is constructing additional water storage tanks to meet the requirement of potable water, and it needs an increase of water supply from the 'Neora Khola Water Supply Scheme' for this purpose.[45] Often, landslides occurring in monsoon season cause havoc to the roads in and around Kalimpong.[46] The West Bengal State Electricity Distribution Corporation Limited (WBSEDCL) provides electricity here.[47] Renewable Energy Development Agency of the state has plans to promote usage of solar street lights in Kalimpong and proposed an energy park here to sell renewable energy gadgets.[48] The Public Works Department is responsible for the road connecting the town to the National Highway–NH-31A.[49] The Kalimpong municipality has a total of 10 health care units, with a total of 433 bed capacity.[50]

 

The Kalimpong assembly constituency, which is an assembly segment of the Darjeeling parliamentary constituency, elects one member of the Vidhan Sabha of West Bengal.[51]

People, culture, and cuisine

The Zang Dhok Palri Phodang monastery atop Durpin Hill

 

The original settlers of Kalimpong are the Lepchas, although the majority of the populace are ethnic Nepali, having migrated from Nepal to Kalimpong in search of jobs while it was under British rule.[52]

 

Indigenous ethnic groups include the Newars, Bhutia, Sherpas, Limbus, Rais, Magars,[53] Chettris, Bahuns, Thakuris, Gurungs, Tamangs, Yolmos, Bhujels, Sunuwars, Sarkis, Damais and the Kamis.[54] The other non-native communities as old as the Nepalese are the Bengalis, Muslims, Anglo-Indians, Chinese, Biharis and Tibetans who escaped to Kalimpong after fleeing the Communist Chinese invasion of Tibet. Kalimpong is home to Trinley Thaye Dorje—one of the 17th Karmapa incarnations.[55] Kalimpong is the closest Indian town to Bhutan's western border, and has a small number of Bhutanese nationals residing here. Hinduism is the largest religion followed by Nijananda Sampradaya, Buddhism and Christianity.[53] Islam has a minuscule presence in this region, The Oldest settlers include people residing since the mid of 19th Century and also mostly Tibetan Muslims who fled in 1959 after Chinese invasion of Tibet.[56] The Buddhist monastery Zang Dhok Palri Phodang holds a number of rare Tibetan Buddhist scriptures.[6] There is a Mosque, Kalimpong Anjuman Islamia Established in 1887 in the bazaar area of Kalimpong.[57]

 

Popular Hindu festivals include Dashain, Tihar, Cultural Programme and the Tibetan festival of Losar. Languages spoken in Kalimpong include Nepali, which is the predominant language; Lepcha, Limbu, Tamang, Kirat, Hindi, English and Bengali.[2] Though there is a growing interest in cricket as a winter sport in Darjeeling Hills, football still remains the most popular sport in Kalimpong.[58] Every year since 1947, the Independence Shield Football Tournament is organized here as part of the two-day-long Independence Day celebrations.[59] Former captain of India national football team, Pem Dorjee hails from Kalimpong.[60]

 

A popular snack in Kalimpong is the momo, steamed dumplings made of pork, beef or vegetable cooked in a wrapping of flour and served with watery soup. Wai-Wai is a packaged Nepalese snack made of noodles which are eaten either dry or in soup form. Churpee, a kind of hard cheese made from yak's or chauri's (a hybrid of yak and cattle) milk, is sometimes chewed.[61] A form of noodle called Thukpa, served in soup form is popular in Kalimpong.[62] There are a large number of restaurants which offer a wide variety of cuisines, ranging from Indian to continental, to cater to the tourists. Tea is the most popular beverage in Kalimpong, procured from the famed Darjeeling tea gardens. Kalimpong has a golf course besides Kalimpong Circuit House.[2][63]

 

The cultural centres in Kalimpong include, the Lepcha Museum and the Zang Dhok Palri Phodang monastery. The Lepcha Museum, a kilometre away from the town centre, showcases the culture of the Lepcha community, the indigenous peoples of Sikkim. The Zang Dhok Palri Phodong monastery has 108 volumes of the Kangyur, and belongs to the Gelug of Buddhism.

 

Media

Kalimpong has access to most of the television channels aired in the rest of India. Cable Television still provides service to many homes in the town and it's outskirts, while DTH connections are now practically mandatory throughout the country. Besides mainstream Indian channels, many Nepali-language channels such as Dainandini DD, Kalimpong Television KTv, Haal Khabar (an association of the Hill Channel Network), Jan Sarokar, Himalayan People's Channel (HPC), and Kalimpong Times are broadcast in Kalimpong. These channels, which mainly broadcast locally relevant news, are produced by regional media houses and news networks, and are broadcast through the local cable network, which is now slowly becoming defunct due to the Indian government's ruling on mandatory digitization of TV channels. The movie production houses like JBU films produces the movies on the nepali and other languages.

 

Newspapers in Kalimpong include English language dailies The Statesman and The Telegraph, which are printed in Siliguri,[65][66] and The Economic Times and the Hindustan Times, which are printed in Kolkata.

 

Among other languages, Nepali, Hindi and Bengali are prominent vernacular languages used in this region.[25] Newspapers in all these four languages are available in the Darjeeling Hills region. Of the largely circulated Nepali newspapers Himalay Darpan, Swarnabhumi and some Sikkim-based Nepali newspapers like Hamro Prajashakti and Samay Dainik are read most.[67] The Tibet Mirror was the first Tibetan-language newspaper published in Kalimpong in 1925.[68] while Himalayan Times was the first English to have come out from Kalimpong in the year 1947, it was closed down in the year 1962 after the Chinese aggression but was started once again and is now in regular print. Internet service and Internet cafés are well established; these are mostly served through broadband, data card of different mobile services, WLL, dialup lines,[69][70] Kalimpong News, Kalimpong Online News, Kalimpong Times and KTV are the main online news sites that collect and present local and North Bengal & Sikkim news from its own agencies like KalimNews and other newspapers. Besides this there are others like kalimpong.info, kalimpongexpress.blogspot.com and several others. All India Radio and several other National and Private Channels including FM Radio are received in Kalimpong.

 

The area is serviced by major telecommunication companies of India with most types of cellular services in most areas.

 

Education

There are fifteen major schools in Kalimpong, the most notable ones being Scottish Universities Mission Institution, Dr. Graham's Homes, St Joseph's Convent, St. Augustine's School, Rockvale Academy, Saptashri Gyanpeeth, Springdale Academy, St. Philomenas School, Kalimpong Girls' High School, Kumdini Homes, Chandramaya High School, Lolay Sampu High School and Gandhi Ashram School. The Scottish Universities Mission Institution was the first school that was opened in 1886. The schools offer education up to high secondary standard, following which students may choose to join a Junior College or carry on with additional two years of schooling.

 

Kalimpong College, Cluny Women's College and Rockvale Management College are the main colleges in the town. Former two are affiliated to the North Bengal University and the latter affiliated to West Bengal University of Technology and apart from these, Good Shepherd IHM (Hotel management Institution) offers courses on hospitality sectors. Most students however, choose to further their studies in Siliguri, Kolkata, and other colleges in the Indian metropolis. The Tharpa Choling Monastery, at Tirpai Hill near Kalimpong, is managed by Yellow Hat sect and has a library of Tibetan manuscripts and thankas.

 

Flora and fauna

The area around Kalimpong lies in the Eastern Himalayas, which is classified as an ecological hotspot, one of only three among the ecoregions of India. Neora Valley National Park lies within the Kalimpong subdivision and is home to tigers.[72] Acacia is the most commonly found species at lower altitudes, while cinnamon, ficus, bamboo and cardamom, are found in the hillsides around Kalimpong. The forests found at higher altitudes are made up of pine trees and other evergreen alpine vegetation. Seven species of rhododendrons are found in the region east of Kalimpong. The temperate deciduous forests include oak, birch, maple and alder. Three hundred species of orchid are found around Kalimpong.

 

The Red panda, Clouded leopard, Siberian weasel, Asiatic black bear,[75] barking deer,[76] Himalayan tahr, goral, gaur[76] and pangolin are some of the fauna found near Kalimpong. Avifauna of the region include the pheasants, cuckoos, minivets, flycatchers, bulbuls, orioles, owls, partridges, sunbirds, warblers, swallows, swifts and woodpeckers.

 

Kalimpong is a major production centre of gladioli in India,[78] and orchids, which are exported to many parts of the world. The Rishi Bankim Chandra Park is an ecological museums within Kalimpong Citrus Dieback Research Station at Kalimpong works towards control of diseases, plant protection and production of disease free orange seedlings.

 

Kalimpong is also famous for their rich practice of cactus cultivation. Its nurseries attract people from far and wide for the absolutely stunning collection of cacti they cultivate. The strains of cacti, though not indigenous to the locale, have been carefully cultivated over the years, and now the town boasts one of the most fascinating and exhaustive collections of the Cactaceae family. The plants have adapted well to the altitude and environment, and now prove to be one of the chief draws of tourism to the township.

 

West Bengal (/bɛŋˈɡɔːl/, Bengali: Paschim Banga [ˈpoʃtʃim ˈbɔŋgo] (About this soundlisten)) is a state in the eastern region of India along the Bay of Bengal. With over 91 million inhabitants, it is the fourth-most populous state and the fourteenth-largest state by area in India. Covering an area of 88,752 km2 (34,267 sq mi), it is also the eighth-most populous country subdivision of the world. Part of the Bengal region of the Indian subcontinent, it borders Bangladesh in the east, and Nepal and Bhutan in the north. It also borders the Indian states of Odisha, Jharkhand, Bihar, Sikkim and Assam. The state capital is Kolkata, the third-largest metropolis, and seventh largest city by population in India. West Bengal includes the Darjeeling Himalayan hill region, the Ganges delta, the Rarh region and the coastal Sundarbans. The state's main ethnic group are the Bengalis, with the Bengali Hindus forming the demographic majority.

 

The area's early history featured a succession of Indian empires, internal squabbling, and a tussle between Hinduism and Buddhism for dominance. Ancient Bengal was the site of several major Janapadas, while the earliest cities date back to the Vedic period. The region was part of several ancient pan−Indian empires, including the Vangas, Mauryans, and the Guptas. The citadel of Gauḍa served as the capital of the Gauḍa Kingdom, the Pala Empire, and the Sena Empire. Islam was introduced through trade with the Abbasid Caliphate, but following the Ghurid conquests led by Bakhtiyar Khalji and the establishment of the Delhi Sultanate, the Muslim faith spread across the entire Bengal region. During the Bengal Sultanate, the territory was a major trading nation in the world, and was often referred by the Europeans as the "richest country to trade with". It was absorbed into the Mughal Empire in 1576. Simultaneously, some parts of the region were ruled by several Hindu states, and Baro-Bhuyan landlords, and part of it was briefly overrun by the Suri Empire. Following the death of Emperor Aurangzeb in the early 1700s, the proto-industrialised Mughal Bengal became a semi-independent state under the Nawabs of Bengal, and showed signs of the first Industrial revolution.[8][9] The region was later conquered by the British East India Company at the Battle of Plassey in 1757 and became part of the Bengal Presidency.[10][11]

 

The region was a hotbed of the Indian independence movement and has remained one of India's great artistic and intellectual centres.[12] Following widespread religious violence, the Bengal Legislative Council and the Bengal Legislative Assembly voted on the Partition of Bengal in 1947 along religious lines into two independent dominions: West Bengal, a Hindu-majority Indian state, and East Bengal, a Muslim-majority province of Pakistan which later became the independent Bangladesh.

 

Post Indian independence, West Bengal's economy is based on agricultural production and small and medium-sized enterprises.[13] For many decades the state underwent political violence and economic stagnation.[14] Today, the economy of West Bengal is the sixth-largest state economy in India with a gross state domestic product (GSDP) of ₹12.54 lakh crore (US$180 billion),[3] and has the country's 23rd-highest GSDP per capita of ₹115,748 (US$1,600).[3] West Bengal also has the 28th-highest ranking among Indian states in human development index, with the index value being less than that of India.[5] The state government debt of ₹4.0 lakh crore (US$56 billion), or 32.6% of GSDP, is fifth highest India, but has dropped from 40.65% since 2010–11.[15][16] There is moderate unemployment.[17] West Bengal has two World Heritage sites and ranks as the seventh-most visited tourist destination in India.

Dog friendly

 

Eating out-of-doors is my favorite. It’s even better when I can bring my dog. Every year, I look forward to sunny days and picnics and frisbee with Jasper.

 

It was a beautiful Sunday for a picnic! I was brave and went, alone, to a meet up with people I didn’t know. I did bring Jasper, though. He was a hit, and, as usual, demonstrated how he is “smarter than the average bear”! (He was also more polite than the average bear and patiently waited for people to spill their food before eating it.)

 

Shirt, Dolce Vita (thrifted). Overalls, Duluth. Shoes, Rocket Dog. Bag, thrifted.

Pretty above average day, craft corner is still tidy from last night, cosplay trousers arrived, sun came out so I basked, and I've booked a bnb for when I'm away in feb!

Only downside was that I was enjoying the first sun of the year so much I ended dup having to do all my work super late in the evening, but cest la vest. It's done now!

Oh hey, and this pic fits in a pile of things!

Sometimes you get satisfaction from taking an average photo when you know the story behind it!

 

Got caught out in a storm this evening and had given up on getting any landscape photos. I managed to get back to the car when I noticed this lone Pelican.

 

It was chucking it down very cold and blowing a gale and my gear was in the car boot, but I thought it was worth the effort so I turned on my headlights to provide some fill light and while being blown around I managed to get a few captures and then lift off!

 

Taken at The Point Bellambi NSW Australia Monday 2nd August 2010.

 

Nikon D700 Nikkor 80-200mm 2.8

Scientific Name: Sericornis magnirostra

Average size: 11cm

In south-eastern Australia, the Large-billed Scrub-wren rarely builds its own nest. Instead it takes over old or disused nests of other birds, particularly that of its larger relative, the Yellow-throated Scrub-wren, sometimes putting down a new lining over abandoned or infertile eggs.

www.birdsinbackyards.net/species/Sericornis-magnirostra

50 zones + average speed cameras = an angry bull!

With this image I conclude the series of shots taken in Southern Italy where, usually, the seeing is on average better than that of the Po Valley. This photo is the sum of 3 photos derotated through the Winjupos program. I used two classic 90-second shots and a 4-minute one that was in turn derotated before adding up.

 

More on: www.astroandnature.com

 

Follow me on instagram: mike_astronature

And I am very happy to be so!

Combined view of fifty photos tagged with "beach", from fifty different Flickr users.

A very average example but I've seen much worse! At least theres no chunks out the side and the paint is good on the rear its all complete which is rare for these

convert *.jpg -average result.jpg

 

Fort Lauderdale is a city in the U.S. state of Florida, 25 miles (40 km) north of Miami. It is the county seat of Broward County. As of the 2019 census, the city has an estimated population of 182,437. Fort Lauderdale is a principal city of the Miami metropolitan area, which was home to an estimated 6,198,782 people in 2018.

 

The city is a popular tourist destination, with an average year-round temperature of 75.5 °F (24.2 °C) and 3,000 hours of sunshine per year. Greater Fort Lauderdale which takes in all of Broward County hosted 12 million visitors in 2012, including 2.8 million international visitors. The city and county in 2012 collected $43.9 million from the 5% hotel tax it charges, after hotels in the area recorded an occupancy rate for the year of 72.7 percent and an average daily rate of $114.48. The district has 561 hotels and motels comprising nearly 35,000 rooms. Forty six cruise ships sailed from Port Everglades in 2012. Greater Fort Lauderdale has over 4,000 restaurants, 63 golf courses, 12 shopping malls, 16 museums, 132 nightclubs, 278 parkland campsites, and 100 marinas housing 45,000 resident yachts.

 

Fort Lauderdale is named after a series of forts built by the United States during the Second Seminole War. The forts took their name from Major William Lauderdale (1782–1838), younger brother of Lieutenant Colonel James Lauderdale. William Lauderdale was the commander of the detachment of soldiers who built the first fort. However, development of the city did not begin until 50 years after the forts were abandoned at the end of the conflict. Three forts named "Fort Lauderdale" were constructed; the first was at the fork of the New River, the second at Tarpon Bend on the New River between the Colee Hammock and Rio Vista neighborhoods, and the third near the site of the Bahia Mar Marina.

 

The area in which the city of Fort Lauderdale would later be founded was inhabited for more than two thousand years by the Tequesta Indians. Contact with Spanish explorers in the 16th century proved disastrous for the Tequesta, as the Europeans unwittingly brought with them diseases, such as smallpox, to which the native populations possessed no resistance. For the Tequesta, disease, coupled with continuing conflict with their Calusa neighbors, contributed greatly to their decline over the next two centuries. By 1763, there were only a few Tequesta left in Florida, and most of them were evacuated to Cuba when the Spanish ceded Florida to the British in 1763, under the terms of the Treaty of Paris (1763), which ended the Seven Years' War. Although control of the area changed between Spain, the United Kingdom, the United States, and the Confederate States of America, it remained largely undeveloped until the 20th century.

 

The Fort Lauderdale area was known as the "New River Settlement" before the 20th century. In the 1830s there were approximately 70 settlers living along the New River. William Cooley, the local Justice of the Peace, was a farmer and wrecker, who traded with the Seminole Indians. On January 6, 1836, while Cooley was leading an attempt to salvage a wrecked ship, a band of Seminoles attacked his farm, killing his wife and children, and the children's tutor. The other farms in the settlement were not attacked, but all the white residents in the area abandoned the settlement, fleeing first to the Cape Florida Lighthouse on Key Biscayne, and then to Key West.

 

The first United States stockade named Fort Lauderdale was built in 1838, and subsequently was a site of fighting during the Second Seminole War. The fort was abandoned in 1842, after the end of the war, and the area remained virtually unpopulated until the 1890s. It was not until Frank Stranahan arrived in the area in 1893 to operate a ferry across the New River, and the Florida East Coast Railroad's completion of a route through the area in 1896, that any organized development began. The city was incorporated in 1911, and in 1915 was designated the county seat of newly formed Broward County.

 

Fort Lauderdale's first major development began in the 1920s, during the Florida land boom of the 1920s. The 1926 Miami Hurricane and the Great Depression of the 1930s caused a great deal of economic dislocation. In July 1935, an African-American man named Rubin Stacy was accused of robbing a white woman at knife point. He was arrested and being transported to a Miami jail when police were run off the road by a mob. A group of 100 white men proceeded to hang Stacy from a tree near the scene of his alleged robbery. His body was riddled with some twenty bullets. The murder was subsequently used by the press in Nazi Germany to discredit US critiques of its own persecution of Jews, Communists, and Catholics.

 

When World War II began, Fort Lauderdale became a major US base, with a Naval Air Station to train pilots, radar operators, and fire control, operators. A Coast Guard base at Port Everglades was also established.

 

On July 4, 1961, African Americans started a series of protests, wade-ins, at beaches that were off-limits to them, to protest "the failure of the county to build a road to the Negro beach". On July 11, 1962, a verdict by Ted Cabot went against the city's policy of racial segregation of public beaches.

Today, Fort Lauderdale is a major yachting center, one of the nation's largest tourist destinations, and the center of a metropolitan division with 1.8 million people.

 

Credit for the data above is given to the following website:

en.wikipedia.org/wiki/Fort_Lauderdale,_Florida

 

© All Rights Reserved - you may not use this image in any form without my prior permission.

 

In an average month when I do not try to limit my spending I pick up a load of doll clothes. It’s a bit like doing drugs – once you started it’s hard to stop (that said, I never did drugs b/c I vastly prefer doll clothes). The reason you get it now and not on the 31st is that I’m trying not to buy more cause this month ended up with an expensive train ticket to visit two of my favorite fellow hobbyists in April :3

 

1. ChuThings Sugar & Coffee [pic by Tna09]

I’m a sucker for ChuThings dresses and especially the ones which consist of only one color. So I hopped on this one like a hyena on carrion (though my postal system seems to have eaten that one up)

 

2. ChuThings for BlytheCon EU Berlin 2012 [pic by supernek]

As far as I found out that set doesn’t have a special name but was released for BlytheCon EU Berlin in quantity of three? And yep, had to get it (to start my ChuThings collection you know).

 

3. Stand Collar Blouse & Salopette Pants Set Beige (PN XS)

4. Sahra's A La Mode Milky Pearl Dress Set Pink (PN M)

Usually I’m shit at catching Azone pre-orders but here I lucked out b/c I saw it in time and got both of the sets I wanted. Now to hope they’ll finally get released and HLJ will bill me /twindles thumbs

 

5. Zolala Babydoll Playsuit Ivory [pic by Zozo]

Woke up to a newsletter informing me of a pre-order for the babydoll playsuits and yes I nearly screamed cause I’ve tried to find one 2nd hand for a while (with no luck) so being able to get one new was an opportunity not to be missed.

 

6. Blue collared dress [pic by iBlythe]

I have the tendency to pick up random bits’n’pieces whilst shopping for the more elaborate sets. They are more often than not rather cheap and make for awesome mix and match items. And this blue dress is terrible cute.

 

7. Valenciennes Baby Doll Bonnet (pic by eBay seller )

I am pretty much addicted to bonnets. That one was listed as pre-1930 on the bay and I have my hopes up that it might fit the doll who is also getting the christening gown shown in my last confession.

 

8. Porter's Chair [pic by Forty Winks Doll Studio]

Not a clothing item but a) I hate white spots in my pics and b) too amazing to be left out (I need a biger dollhouse for all the playscale furniture I accumulate)

My vava (no.3) is home! I'm so excited and my hands literally shakes when I opened her box. It's my dream comes true to have her with sleepy eyes and teeth. I can't even say....

Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.

 

The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.

 

Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.

 

As stated in the foundation document in U.S. National Park Service website:

 

The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.

 

The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.

 

The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.

 

As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.

 

Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.

 

Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.

 

Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.

 

The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.

 

The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.

 

A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.

 

In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.

 

In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.

 

In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".

 

Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.

 

Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.

 

Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.

 

Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.

 

Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.

 

American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.

 

An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.

 

A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.

 

Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.

 

Among the notable features of the park are the following:

Balanced Rock – a large balancing rock, the size of three school buses

Courthouse Towers – a collection of tall stone columns

Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail

Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park

Devils Garden – many arches and columns scattered along a ridge

Double Arch – two arches that share a common end

Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)

Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)

Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area

The Phallus – a rock spire that resembles a phallus

Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008

The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.

 

Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.

 

Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.

 

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

 

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.

 

The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.

 

Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.

 

The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:

 

use of the bow and arrow while hunting,

building pithouse shelters,

growing maize and probably beans and squash,

building above ground granaries of adobe or stone,

creating and decorating low-fired pottery ware,

producing art, including jewelry and rock art such as petroglyphs and pictographs.

 

The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.

 

These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.

 

In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.

 

In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.

 

Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.

 

At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.

 

The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.

 

A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.

 

Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.

 

Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.

 

Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.

 

Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.

 

Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.

 

The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.

 

Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.

 

Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.

 

In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.

 

The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.

 

Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.

 

After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.

 

As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.

 

Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.

 

Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.

 

Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.

 

Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.

 

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.

 

Main article: Latter Day Saint polygamy in the late-19th century

During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.

 

The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.

 

Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:

 

William Torrington in Carson City (then a part of Utah territory), 1859

Thomas Coleman (Black man) in Salt Lake City, 1866

3 unidentified men at Wahsatch, winter of 1868

A Black man in Uintah, 1869

Charles A. Benson in Logan, 1873

Ah Sing (Chinese man) in Corinne, 1874

Thomas Forrest in St. George, 1880

William Harvey (Black man) in Salt Lake City, 1883

John Murphy in Park City, 1883

George Segal (Japanese man) in Ogden, 1884

Joseph Fisher in Eureka, 1886

Robert Marshall (Black man) in Castle Gate, 1925

Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).

 

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

 

Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.

 

During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.

 

In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.

 

Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.

 

Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.

 

As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.

 

One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.

 

It is estimated that 1,450 soldiers from Utah were killed in the war.

Average example the badge isn't too great but it is all complete on the rear and I'm sure it will clean up nicely so a good find

A very average example I've been finding a lot of these recently but its not a problem as i can sell it on the rear its all complete

Hookipa

Carrieton.

The Carrieton district has a highly unreliable but average rainfall of around 300mm per annum and the elevation at 395 metres (or 1,300 feet) made it an attractive area for early pastoralists. The town of Carrieton stands on what was part of the Yanyarrie Run. In 1853 the Grants sank a well and built a large stone tank around- the Yanyarrie Whim which is located on the northern outskirts of Carrieton. Yanyarrie Run and Coonatto Run made up the main runs of the Grant brothers. By 1859 the combined runs exceeded 900 square miles. In 1866 the Grants bought property near Millicent for pasturage during times of drought. This was needed in that year as in 1864 they had shorn 87,000 sheep but in 1866 they only had 18,000 to shear. Their wool was carted by bullock dray down to Port Augusta through Horrocks Pass. Another run in the district was Yalpara Run east of Carrieton run by John and Richard Ragless. They had their own desalination water plant in the 1870s to make the well water potable. They faced tough years and during the drought of 1866 half of their 250,000 sheep died. Their run, like the Grants runs was resumed in 1875.

 

Despite being many miles beyond Goyder’s Line (even Orroroo was beyond Goyder’s Line) the government resumed this section of the Grant family runs in 1877 to survey the Hundred of Yanyarrie and establish the government towns of Carrieton and Eurelia. Both towns had settlement begin around 1878 just a couple of years before the railway to Quorn was pushed through the area in 1881. With the land sales the Grants bought some freehold land and maintained a small station on Coonatto finally selling up in 1903. As one local newspaper reported in 1880 before the droughts set in “farmers will reach the banks of the Finke River and the McDonnell Ranges”! But 1882 proved Surveyor General George Goyder correct. The grain and the top soil blew away in a terrible drought throughout this region. It was a terrible start to the little towns of Carrieton and Eurelia. Yet they survived.

 

By 1879 Carrieton had a post office, a general store, Davies blacksmiths and coach builders- the largest operations north of Gawler. (In 1890 this business employed 31 men in Carrieton.) The Carrieton Hotel opened in 1879 with Michael O’Grady being the first publican. The Eureka Hotel opened in 1880, but closed in 1946 and was then demolished. When the government conducted a census in 1881 Carrieton had a population of 120. (Today it has less than 100 people.) By then it had a railway siding and railway station which opened in 1880. Carrieton was an important stop as the carriage lamps were all taken out at Carrieton to have their wicks cleaned and trimmed and the lamps polished before being replaced in the next train. In the early 1880s during the drought Carrieton acquired a school (1882), a police station (1884), St Raphael’s Roman Catholic Church (the large presbytery was built in 1889), a small Methodist Church (1882), an Anglican Church (1888) and the railway station, built in 1885 at a cost of £1,500. The first agricultural show was held in Carrieton in 1882. These days the town has an annual night time rodeo which started in 1953. But Carrieton is very much a ghost town. The hotel recently closed, the school is a private residence, the churches are used for housing as is the railway station and the old stores are derelict and falling down. The town has no future.

 

Just your average, typical day during Okinawa's Summer.

One of the first things I noticed as a young Marine on Okinawa was the clouds. Every day, you can expect high level cirrus clouds, along with small nimbus clouds the seem to form at the Southern part of Okinawa and work their way up the island. Much different from what we see here in MIchigan. And Okinawa's clouds always make a good photogragh, even during flat lighting.

 

Shot from the next town West of Nago. Yabu is the name?

 

Taken with my X-700, 19-35mm Vivitar, Kodak Elite Chrome, Marumi polarizer

More average seeing, but I keep on trying, hoping for a night of better conditions.Air quality had improved from yesterday, but the smoky haze remained higher up, again dimming the planet and making images appear orange before performing a colour balance.

average of all daily photos published aug 2016

 

total exposure time in seconds: 1.8052179111

thinks he isn't :-) Father Larry Lorenzoni. HBW!!

pyracantha, 'Cadune', j c raulston arboretum, ncsu, raleigh, north carolina

Average depth of 100 m deep, glacier water 4 °C

Jasper NP, the largest national park in the Canadian Rocky Mountains.

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

Durchschnittliche Tiefe von 100 m, Gletscherwasser 4 °C

Jasper NP, der größte Nationalpark in den kanadischen Rocky Mountains.

this lady is not so hot. nevertheless she is very pure

Metroline DE1599 (YX58DUH) is seen at Ruislip Station on route U1

 

Formerly First London DML44023

Best viewed in lightbox - please click on the image or press L.

 

Z to zoom in.

  

© All rights reserved R.Ertug

Please do not use this image without my explicit written permission.

 

Spring and fall are the best times of year for sightseeing in Istanbul. The weather is pleasant, with comfortable temperatures averaging around 15°C. While spring is high season in Istanbul, crowds don’t reach their peak until late May. In the fall, the number of tourists who arrive begins to dwindle, with the crowds thinning by early October. Many feel that spring is the best time of all, and particularly April, when the entire city is in bloom for the International Tulip Festival held throughout the month. Still, autumn is the time when the city comes alive in a gamut of colors, both somber and bright, while the light rain and glorious sunsets make for an impressionist painting of sorts. When visiting in the spring, summer or fall, the most pleasant time to experience Istanbul’s top sights is early in the morning, soon after opening, or late in the day. Popular Topkapi Palace is best visited on a Monday morning when it’s usually at its quietest. In winter, you can usually arrive at any time and find no queue or crowds. Summer is just the opposite, arguably the worst time to visit due to the sweltering heat, massive amounts of people visiting the city, and the lines for attractions and other tourist sites. As the major sights in Istanbul all have their own closing days and slightly different operating hours, be sure to check with each one before planning your itinerary.

 

EMIRGAN PARK -

  

The Emirgan Park is a historical urban park located at the Emirgan neighbourhood in the Sarıyer district of Istanbul, Turkey, on the European coast of the Bosphorus. It is one of the largest public parks in Istanbul.

 

In the Byzantine era, the entire area, where today the park stretches, was covered with cypress trees and known as "Kyparades" or "Cypress Forest". It became known as "Feridun Bey Park", when the uninhabited land was granted in the mid-16th century to Nişancı Feridun Bey, a Lord Chancellor in rank in the Ottoman Empire.

 

In the 17th century, Ottoman sultan Murad IV (reigned 1623-1640) presented the estate to Emir Gûne Han, a Safavid Persian commander, who surrendered his sieged castle without any resistance, and followed him back to Istanbul. The name "Feridun Bey Park" was changed to "Emirgûne", which in time became corrupted to "Emirgan".

During the centuries, the estate's owner changed several times, and by the end of the 1860s, it was owned by Khedive Ismail Pasha (reigned 1863-1879), Ottoman governor of Egypt and Sudan. The area was used as the backyard of a large wooden yalı that he built on the shore of the Bosphorus. Further, he built within the park area three wooden pavilions, which still exist.

The heirs of the Khedive's family sold the estate in the 1930s to Satvet Lütfi Tozan, a wealthy Turkish arms dealer, who granted the park grounds, the three pavilions included, later in the 1940s to the City of Istanbul during office of Governor and Mayor Lütfi Kırdar (1938-1949).

 

The park today-

 

A pond with fountain in the Emirgan Park

The park, owned and administered today by the Metropolitan Municipality of Istanbul, covers an area of 117 acres (470,000 m2) on a hillside, and is enclosed by high walls.

Inside the park with two decorative ponds are plants of more than 120 species. The most notable rare trees of the park's flora are: Stone Pine, Turkish pine, Aleppo Pine, Blue Pine, Eastern White Pine, Maritime Pine, Japanese Cedar, Norway Spruce, Blue Spruce, Atlas Cedar, Lebanon Cedar, Himalayan cedar, Beech, Ash tree, Sapindus, Babylon Willow, Hungarian Oak, Colorado White Fir, Maidenhair tree, California incense-cedar, Coast Redwood and Camphor tree.

Many jogging tracks and picnic tables make the Emirgan Park a very popular recreation area for the local people, especially during the weekends and holidays.The three historic pavilions, called after their exterior color as the Yellow Pavilion, the Pink Pavilion and the White Pavilion were restored in time between 1979-1983 by the Touring and Automobile Club of Turkey under its CEO Çelik Gülersoy, and opened to the public as cafeteria and restaurant.

The Emirgan Park is closely associated with the tulip, the traditional flower, which gave its name to an era (1718-1730) of the Ottoman Empire. A special garden was established in Emirgan Park in the 1960s to revive the city's tradition of tulip cultivation. Since 2005, an annual international tulip festival is organized here every April making the park attractive and very colorful with these flowers.

  

The Yellow Pavilion - Sarı Köşk is a large wooden mansion in the form of a chalet built by Khedive Ismail Pasha between 1871-1878 as a hunting lodge and guest house.

Situated in the center of the park and overlooking the Bosphorus, the two-storey mansion with one balcony, one terrace and a basement is constructed on an area of 400 m2 (4,300 sq ft). It consists of four rooms, one hall and a kitchen in the lower floor and three rooms and one salon in the upper floor. Its layout reflects the architecture of the traditional Ottoman house with a salon encircled by many living rooms.

 

The ornaments at the ceilings and the walls were the work of the court architect Sarkis Balyan. The ceilings are enriched with oil painted flower figures and the facades with outstanding carvings. The high doors and windows, as well as the opulent interior decorations in bright colors reflect the glory of that era.

A pond is situated to the northeast, next to the mansion.

Used only by the owners from the very beginning, the pavilion was restored within four months in the beginning of the 1980s with due diligence, furnished with antiques and opened to the public as a cafeteria.The Yellow Pavilion, the main base of the park, is run since 1997 by Beltur, the tourism company of the Metropolitan Municipality of Istanbul. Up to 100 guests can be served at the premise in summer and winter time.

 

The Pink Pavilion - Pembe Köşk, one of the three mansions in the park built by Khedive Ismail Pasha, is a two-storey, typical Ottoman house. Named after its exterior's original color of cranesbill flower pink, the pavilion reflects the glory of its history with fine ornaments.

The pavilion is used as a cafeteria on weekends. Furthermore, it available for conventions and wedding ceremonies. In the summer months, the premise can accommodate up to 350 guests, for cocktails up to 500 people. In the winter time, groups of up to 150 guests can be served.

  

The White Pavilion - Beyaz Köşk is the third mansion within the Emirgan Park built by Khedive Ismail Pasha. It is only 150 m (490 ft) far from the Yellow Pavilion. The two-storey wooden building bears the architectural characteristics of the neo-classical style.

The mansion is used in the daytime as a cafeteria and in the evenings as a restaurant of Turkish-Ottoman cuisine.

  

"The Quinault Valley receives an average of 12 feet of rain per year that maintains the temperate rain forest ecosystem. This short trail is an excellent introduction to some of the lush and dense forest growth in this section of Olympic National Park."

"You'll walk through lush bigleaf maples and ferns on the first part of the trail. Once you reach Kestner Creek, this is where you'll see more mosses, ferns and spike-mosses growing on the trees. It's a beautiful moss-draped forest. Dominate species are Sitka spruce and western hemlock, but other species grow as well. Many trees are 100 years old. You can see many bigleaf maples on the last part of the trail, but you'll also find nurse logs and dead wood that line the trail." www.outdoorproject.com

 

"Covering nearly one million acres, Olympic National Park provides three distinct ecosystems—glaciated mountains, rugged Pacific coastline, and lush temperate forests—and their distinct flora and fauna for nature-lovers to explore. Over 95% of the park is designated wilderness, protecting one of the largest wilderness areas in the lower 48, giving visitors the opportunity to experience remoteness and pristine nature in a way that few other places can."

"The 73-mile long coastline has rocky headlands, sandy beaches, thriving tidepools, erosion-formed offshore sea stacks, that provide habitats to marine and intertidal wildlife. The diverse forest communities making up the park provide homes to everythings from acid-loving wild cranberry bushes to giant spruce trees, hundreds of years old. The towering mountain ranges created by tectonic collision are topped with ancient glaciers." www.nationalparks.org

Average of four exposures to extend exposure and reduce noise, a slight contrast tweak, that's all.

 

Taken from outside the door of our holiday house.

 

Mr. and Mrs. Sven Djars, son Erik...and a puppy too :)

We're finally here with our female "AVERAGE" body skin. This body skin is compatible to the listed mesh bodies. Any other mesh bodies, please try demo before purchasing. More body skins will come into the future as we progress with different variations.

 

*BOM LAYERS ONLY*

 

UBER:

maps.secondlife.com/secondlife/SKYLINE%20DREAMS/56/31/3742

All rights reserved by giglens

Average depth of 100 m deep, glacier water 4 °C

Jasper NP, the largest national park in the Canadian Rocky Mountains.

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

Durchschnittliche Tiefe von 100 m, Gletscherwasser 4 °C

Jasper NP, der größte Nationalpark in den kanadischen Rocky Mountains.

...in a home in the US is about 40-45 psi. The things I learn working on a research project.

 

Processed with VSCOcam with b4 preset

average looking plane, average looking scheme.

Skulptur von Tony Cragg, Bonn Remigiusplatz

Holy crap hey back out shooting and loving it again. 2013 was a pretty average year for my family and myself in a lot of ways. I didn't know whether I was coming or going, especially with my photography. At one point I was dead set going to just be done with it and sell all my gear and purely focus on my surfing.

I only held off solely on what a few good friends said, and I'm glad I did.

the passion for taking photos has touched me once again. Still a bit rusty but its all starting to come back.

I've had most of my recent posts in mind for the past two years,even scouted them as far back as that. Now with my new found enthusiasm I'm revisiting them this time with camera in tow ready to shoot.

Hope your not getting to bored of all the posts but I have a lot to catch up on and a few spots still to go and capture.

thanks to all that kept in my ear about not giving it away and to all of you who view and comment on my shots.

Big Cheers.

Family: Phoenicopteridae

Length: 1.2 to 1.45m Wingspan: 1.4 to 1.7m Weight: 3 to 4kg (Males tend to be larger than females). Lifespan: Averaging between 30 to 40 years. (In captivity, The Greater Flamingo has been known to live 50 to 60 years plus).

This is the largest living species of Flamingo and is found in parts of North Africa, Southern Asia, (mainly around the coastal regions of India and Pakistan). In Europe, they are more locally around the Southern parts of Europe, from Spain, Portugal, along the coastal regions of Southern France, as well as other southern and Eastern countries, bordering on the Mediterranean coast line; also found in the Middle Eastern countries.

Habitat: Found in a variety of saltwater habitats, especially shallow coastal lagoons, salt pans, mudflats, also alkaline lakes. Flamingos maybe even be seen feeding from freshwater inlets and lakes.

Some of the Flamingos natural habitats are under threat, mainly due to building developments close by, especially pollution from manufacturing Industries that produce chemical wastes. When pollution is spilled into their natural water supplies, the habitat can instantly die!

Here in Spain, The Greater Flamingo (Phoenicopterus ruber) are seen in large numbers on the Salt lakes in Santa Pola, Alicante. (Incidentally this is where most of these images were taken from).

Flamingos are social birds, they will be seen mainly in flocks, (Flamingo flocks are referred to as a ‘colony,’ or a ‘stand’).

Feeding:

Greater Flamingos are omnivores and are filter-feeders. They usually feed head submerged, with its bill upside down, sieving through the shallow water for small crustaceans. This is achieved by sucking in the water through the partly closed bill, the water is then pushed out by pumping their tongue up and down continuously, (about 5 to 6 times a second) this can last up to 20 seconds while the head is still submerged. It was fascinating observing them as they scuffle their feet, disturbing the underwater sediment, for tiny crustaceans, such as shrimp, molluscs, tiny fish, plankton and insect larvae. Plant material is also eaten, such as decaying leaves, algae, seeds, and small young water plants.

While observing I did notice that each bird (if not paired up) preferred their own “elbow” space. The odd peck, scuffle or short chase did occur occasionally, especially if one came too close to another, while it was feeding.

The immature Flamingo lacks the mature Flamingos colourful, pinkish-white body plumage and red wing coverts; also lacking the colourful pink bill, with a black tip. The adults attain their colourful plumage, which mainly comes from their diet of shrimp and other pink crustaceans, living in the warm saltwater.

Nesting: April to May. Consisting of a small pillar/mound of mud, constructed in shallow water, usually safe from land-based predators. One chalky-white egg is laid, both parents take it in turn to incubate the egg, which usually takes between 27 to 31 days to hatch. While the chick is hatching, the parents will help the young chick to break away the shell.

Flamingo nests are plundered, mainly by seagulls, raptors, crows and I suspect herons and egrets will also take the opportunity if a nest is left unattended. Chicks are covered mostly in grey with some white, fluffy down. The new born chick being more vulnerable to predation, in their early days of life. The Chick will be fed entirely by both parents for up to four weeks or more. While feeding, both parents produce a rich creamy pink liquid, this is known as “crop-milk”. A chick will fledge around ten weeks but will remain in the “flamingo creches” for another month. Each chick has its own unique call, remarkably the parent birds are able to distinguish their chicks call, amongst hundreds and sometimes thousands of other young chicks, that are grouped together in these “flamingo creches”. Flamingos have just one brood/chick a year.

 

Flamingo chicks are grey and white when born and do not develop their pink colouration for around 2 years. The chick is fed for at least the first 3 – 4 weeks entirely by the parents who secrete a creamy pink liquid called ‘crop milk’ which comes from the parents upper digestive tract. Either parent can feed the chick this way and other flamingos can act as foster feeders.

The chicks fledge after 10 weeks, but remain in creches for a further month. The chick is born with a straight bill which starts to curve at about one month and can filter feed properly at two and a half months. Amazingly, the adult flamingo is able to locate its chick from hundreds or thousands of other chicks, by its ‘call’.

Flamingos are fully grown at 2 years and are able to mate at 3 years. Most flamingos will not breed for the first time until they are 5 to 10 years old. Flamingos may not breed when wetlands are dry and food is scarce. Some years, their feeding pools are teeming with life and there is plenty of food with which to feed their chicks. However, other years the pools are nearly empty. As a result, flamingos may only breed when conditions are just right.

The Greater Flamingo can live to the age of over 60 years old in captivity. The average life span in the wild is around 30 – 40 years.

The average adult dog sleeps 12 to 14 hours per day. However, The amount of sleep a dog needs depends on their age, breed, and activity level. Chicca was 9 years old in this picture. That's approximately 63 years in human years, so she is fast approaching what is considered a "Senior age dog". She naps alot.

 

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ASK THE AVERAGE YOUNG CITIZEN walking around Hamilton what happened on the "Mountain" during WW II and you'll get blank stares.

 

What was CANADA doing on the Mountain, peeps … when Herr Hitler was trying to take over the free world?

 

Not a clue.

 

In what would become the largest training endeavour, ever mounted by a single nation, let alone a small country like Canada, "The British Commonwealth Air Training Plan (BCATP)" was launched in 1939 earmarking CANADA as its' BIGGEST PARTICIPANT and HEADQUARTERS of the British led operation.

 

And by the early 40s … the BCATP had finally come to Hamilton (see Picture above).

 

What exactly was the BCATP?

 

THE BRITISH COMMONWEALTH AIR TRAINING PLAN (BCATP, or "The Plan) was a "MASSIVE, JOINT MILITARY aircrew training program created by the UK, Canada, Australia, and New Zealand during the Second World War" (Steven Haytor). South Africa and Southern Rhodesia later participated, somewhat individually, in the "The Plan" as well.

 

Canada, far from Nazi bombers, with predictable weather, large areas of undeveloped land, and located next door to the industrial American giant (with an endless supply of planes and parts) … was the ideal location for such a challenging endeavour. By the end of the Plan in 1945, the young Dominion of Canada had trained 131, 533 pilots, and aircrew. Only 72, 835 of these, just over half, were Canadian.

 

The rest of the trainees came from everywhere. The UK. The USA. Australia, New Zealand, Poland, Norway, the Free French of France (and elsewhere), Holland, Belgium, Czechoslovakia, and Denmark.

 

Since aircrew training centres were located right across Canada, "The Plan", ended up unifying Canada like no other event had … since, maybe the Last Spike was driven into the Canadian Pacific Railway on November 7, 1885, in Craigellachie, BC.

 

The CPR railway physically united the country, back in the day, but Canada would have to wait until the British Commonwealth Air Training Plan … before the hearts and minds of Canadians were united against a very real and ominous threat which could have changed Canada forever, and for the worse.

 

In 1939, the Prime Minister of Canada, Mackenzie King, had a dream that he took as a sign. It became for him, a premonition of "the power of the airplane in determining (the) ultimate victory (of the war)". So when the British government went looking for help from its' Commonwealth countries, to train sizeable Allied aircrews for the war, King couldn't sign up Canada, fast enough.

 

FULL STOP.

 

Folks, this was a HUGE undertaking!

 

CANADA had signed on and was now expected to turn out 50,000 trained pilots and aircrew, for every year of the BCATP operation! Until the Allies prevailed.

 

More than a 100 aerodromes needed to be built including hundreds of runways, and hundreds of hangars.

 

Several hundreds of buildings also still had to built when Canada signed the 1939 BCATP agreement.

 

And, to complicate things further … over 100,000 training and support services men and women also had to be trained, and then dispersed to these training facilities as well. My dad was one such person.

 

"The free world needed a champion and Canada answered the call!"

 

On the third anniversary of the successful operation of the British Commonwealth Air Training Plan, President Roosevelt (FDR) wanted to send a letter of congratulation to our Prime Minister King. The BCATP trained aircrews had contributed significantly to the Allied air dominance in the air war over Europe, and in the South-east, and expectedly this achievement was a source of great Canadian pride.

 

Every community in Canada was involved in one way or another with "The Plan". So, to mark the glorious milestone, the White House contacted (future PM) Lester B. Pearson who was in Washington at the time. It was pressed upon L.B. to ghost write a message from the US president … to the Canadian prime minister.

 

The US State Department always handles these sorts of things.

 

But, not this time.

 

On January 1, 1943, Prime Minister King got Lester B.'s ghost letter, signed and obviously approved of, by President Roosevelt. Yes, Canada was congratulated by the world famous FDR in this letter for having become the "Aerodrome of Democracy". The letter, went on, of course, to make headlines everywhere.

 

As I wrap this up I wanted to note, while the Commonwealth countries had agreed to, and had shared the cost of the BCATP, it was discovered, at war's end, that Great Britain still owed Canada a vast amount.

 

$425 million dollars.

 

Using an inflation calculator, that's a cool 7.0 billion Canadian dollars today!

 

And this huge sum … was expected to come from, a depleted, and broke Britain? That's a LOT of owed money, folks!

 

In March of 1946, Canada canceled Britain's debt to our nation and absorbed the outstanding war debt itself.

 

Finally, and also to be noted, Canadian communities welcomed the far-flung trainees when they arrived, far from home.

 

Summer fairs and winter carnivals were recreational events that always unified Canadian communities perennially, but most certainly these events, when the world was at war, amplified community and military morale with the new international participation!

 

Many of these boys, trained right here in Canada, would enter air combat (shortly after their BCATP training) and would be killed in action. Never to return home. This was a very sobering reality.

 

Therefore, sports events and competitions, as well as dances were set up for these "temporary Canadians" to help reduce their stress and to enjoy their stay in the greatest country on earth.

 

Participation in community organized events provided relief for these future airmen, offsetting their grueling flight training schedules. These RCAF station events were open to the whole civilian host communities, and not just the military folk … as were the final military presentation of wings, and graduation ceremonies.

 

And whenever these mass gatherings of men and women occur, and war is on, and the time is short … we can be sure that more than one airman left his heart at RCAF Station Fingal, RCAF Station Hamilton, RCAF Station Centralia, etc.

 

And more than one Canadian woman pined her heart away … for the airman who never returned.

 

FYI over 3,750 airmen of the RAF, RAAF, RNAF took Canadian wives and most of these women moved away to join their husbands in distant Commonwealth lands, though some grooms later settled back in Canada.

 

Many airports around Canada, both large and small, were once BCATP locations!

 

RCAF STATION HAMILTON ::: British Commonwealth Air Training Plan participation:

 

No. 10 Elementary Flying Training School (No. 10 EFTS), Aircraft: De Havilland Tiger Moth and Fleet Finch

 

No. 33 Air Navigation School (No. 33 ANS), Aircraft: Avro Anson

 

AFTER THE WAR, Hamilton 424 Reserve Squadron was based at Mount Hope and flew the P-51 Mustang and the De Havilland Vampire jet fighter under AIR DEFENCE COMMAND.

 

Later, under AIR TRANSPORT COMMAND 424 Squadron flew Beechcraft Expeditor and the De Havilland Otter.

 

Other units were also located in Hamilton such as No. 16 Wing (Auxiliary), No. 2424 Aircraft Control and Warning Squadron (Auxiliary) trained Pinetree Line radar operators, and the Royal Canadian Naval Reserve's No. 1 Training Air Group.

 

NATO Air Training that occurs in Canada TODAY became a natural extension from the success of The British Commonwealth Air Training Plan program. Most of these Canadian NATO-Affiliate training locations were former BCATP airfields.

 

One province, Newfoundland, however, did not participate in the BCATP because it did not become a part of Canada until 1949, long after WW II ended.

 

AV ENTHUSIASTS … note the B-25 on the tarmac, BOTTOM CENTRE.

 

(Recently I came across this YHM airfield photo from the 1940s. I straightened it, enlarged it significantly, colourized it, brightened it and added identifying text with a banner. Cheers!)