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Former Kroger of Elizabethton, TN also featuring the adjacent Auto Zone which was likely a Super X drug store originally
3 differing forms of stock movement along the Hume Highway heading south towards Yass.
(1/3) Single drive Southern Cross Horse Transport MAN with the bloodstock on board.
(2/3) The great small and local transporter, FUSO, unbranded livery but doing its job well.
(3/3) Ross Smith Livestock Transport out of Wagga with the woolies in tow behind the KENWORTH.
New South Wales, Australia.
Il sogno è vedere le forme invisibili della distanza imprecisa, con sensibili movimenti della speranza e della volontà cercare
sulla fredda linea d'orizzonte
l'albero, la spiaggia, il fiore, l'uccello, la fonte: i baci meritati della Verità. (Fernando Pessoa)
Corsica : Coast of Balagna seen from the beach of Nonza (Capi Corsu)
Van's US Open 2014 Huntington Beach with pro surfers Alana Blanhard, Lakey Peterson, Laura Enever, Sally Fitzgibbons, Coco Ho, Stephanie Gilmore, newcomers Nikki Van Dijk and Tatiana Weston-Web, and more!
The new Nikon D810 rocks for sports photography! New Instagram!
Goddess videos! vimeo.com/45surf
Nikon D810 Photos Pro Women's Surfing Van's US Open Sports Photography Tamron SP 150-600mm F/5-6.3 Di VC USD !
I shot in DX mode which crops away the extra pixels and takes me 1.5X closer while allowing for up to 7 FPS with the Nikon D810's Nikon MB-D12 Battery Grip using the 8 AA battery option! 8 Duracles took me through around 3,000 shots no problem--maybe more! I was shooting at the equivalent of 900mm with the 1.5x crop factor! Pretty close! Had I gone with the Nikon D4s, I would have gotten 12 fps, but no DX crop factor, as the sensor has only around 14mp, compared to the d810's 36 megapixels! Sure the larger pixel size on the Nikon D4s full frame sensor comes in handy indoors or at night, but in the brigth sun, there's more than enough light for the smaller pixels in crop mode! Sure we lose some pixels from the outer edges when shooting in DX crop mode, but most of those pixels would be cropped away in lightroom anyway. And the smaller files make the memory cards last longer, while also upping the FPS to 7 shots per second! Not quite 12 FPS< but still awesome and enough I felt!
What a beautiful way to test the Nikon D810 and Tamron 150-600mm zoom lens for sports photography!
Athletic graceful girl goddesses! Tall, thin, fit and in shape! Pro women's surfers form the van's us open wearing both long wetsuits and bikini bottoms with shorty wetsuit tops/summer wetsuits. Sexy, beautiful beach babes and water goddesses all! Many are professional swimsuit bikini / surf lifestyle models too!
Tamron SP 150-600mm F/5-6.3 Di VC USD Autofocus lens for Nikon AF-D Cameras.
The new Nikon D810 rocks for sports photography New Instagram!
Seaforth Radar Station, in the current form, was built in 1969 as a result of the construction of Royal Seaforth Dock.
++++++ FROM WIKIPEDIA ++++++
Kathmandu (/ˌkætmænˈduː/;[2] Nepali: काठमाडौँ, Nepali pronunciation: [ˈkaʈʰmaɳɖu]) is the capital and largest city of Nepal, with a population of around 1 million. Also known as the city of temples, the city stands at an elevation of approximately 1,400 metres (4,600 feet) above sea level in the bowl-shaped Kathmandu valley in central Nepal. The valley was historically called the "Nepal Mandala" and has been the home of the Newar people, a cosmopolitan urban civilization in the Himalayan foothills. The city was the royal capital of the Kingdom of Nepal and hosts palaces, mansions and gardens of the Nepalese aristocracy. It has been home to the headquarters of the South Asian Association for Regional Cooperation (SAARC) since 1985. Today, it is the seat of government of the Nepalese republic, established in 2008, and is part of the Bagmati Province.
Kathmandu is and has been for many years the centre of Nepal's history, art, culture, and economy. It has a multi-ethnic population within a Hindu and Buddhist majority. Religious and cultural festivities form a major part of the lives of people residing in Kathmandu. Tourism is an important part of the economy in the city. In 2013, Kathmandu was ranked third among the top ten upcoming travel destinations in the world by TripAdvisor, and ranked first in Asia. The city is considered the gateway to the Nepalese Himalayas and is home to several world heritage sites: the Durbar Square, Swayambhunath, Boudhanath and Pashupatinath. Kathmandu valley is growing at 4 percentange per year according to the World Bank in 2010, making it one of the fastest-growing metropolitan areas in South Asia, and the first region in Nepal to face the unprecedented challenges of rapid urbanization and modernization at a metropolitan scale.
Historic areas of Kathmandu were severely damaged by a 7.8 magnitude earthquake in April 2015. Some of the buildings have been restored while some remain in the process of reconstruction.
Etymology
The indigenous Newari term for Kathmandu valley is Yen. The Nepali name Kathmandu comes from Kasthamandap, which stood in the Durbar Square. In Sanskrit, Kāṣṭha (Sanskrit: काष्ठ) means "Wood" and Maṇḍapa (Sanskrit: मण्डप) means "Pavilion". This public pavilion, also known as Maru Satta in Newari, was rebuilt in 1596 by Biseth in the period of King Laxmi Narsingh Malla. The three-storey structure was made entirely of wood and used no iron nails nor supports. According to legends, all the timber used to build the pagoda was obtained from a single tree.[4] The structure collapsed during a major earthquake in April 2015.
The colophons of ancient manuscripts, dated as late as the 20th century, refer to Kathmandu as Kāṣṭhamaṇḍap Mahānagar in Nepal Mandala. Mahānagar means "great city". The city is called Kāṣṭhamaṇḍap in a vow that Buddhist priests still recite to this day. Thus, Kathmandu is also known as Kāṣṭhamaṇḍap. During medieval times, the city was sometimes called Kāntipur (Sanskrit: कान्तिपुर). This name is derived from two Sanskrit words – Kānti and Pur. Kānti is a word that stands for "beauty" and is mostly associated with light and Pur means place, thus giving it the meaning, "City of light".
Among the indigenous Newar people, Kathmandu is known as Yeṃ Deśa (Nepal Bhasa: येँ देश), and Patan and Bhaktapur are known as Yala Deśa (Nepal Bhasa: यल देश) and Khwopa Deśa (Nepal Bhasa: ख्वप देश) respectively.[5] "Yen" is the shorter form of Yambu (Nepal Bhasa: यम्बु), which originally referred to the northern half of Kathmandu. The older northern settlements were referred to as Yambi while the southern settlement was known as Yangala.[6][7]
The spelling "Katmandu" was often used in older English-language text. More recently, however, the spelling "Kathmandu" has become more common in English.
History
Archaeological excavations in parts of Kathmandu have found evidence of ancient civilizations. The oldest of these findings is a statue, found in Maligaon, that was dated at 185 AD.[9] The excavation of Dhando Chaitya uncovered a brick with an inscription in Brahmi script. Archaeologists believe it is two thousand years old.[9] Stone inscriptions are a ubiquitous element at heritage sites and are key sources for the history of Nepal.
The earliest Western reference to Kathmandu appears in an account of Jesuit Fathers the Portuguese Jesuit, Fr. Joao Cabral who passed through the Kathmandu Valley in the spring of 1628 [10]and was received graciously by the king of that time, probably King Lakshminarasimha Malla of Kathmandu on their way from Tibet to India,[11] and reported that they reached "Cadmendu", the capital of Nepal kingdom.[12]
Ancient history
The ancient history of Kathmandu is described in its traditional myths and legends. According to Swayambhu Purana, present-day Kathmandu was once a huge and deep lake named "Nagdaha", as it was full of snakes. The lake was cut drained by Bodhisatwa Manjushree with his sword, and the water was evacuated out from there. He then established a city called Manjupattan, and made Dharmakar the ruler of the valley land. After some time, a demon named Banasur closed the outlet, and the valley again turned into a lake. Then Lord Krishna came to Nepal, killed Banasur, and again drained out the water. He brought some Gopals along with him and made Bhuktaman the king of Nepal.[13][14][15]
Kotirudra Samhita of Shiva Purana, Chapter 11, Shloka 18 refers to the place as Nayapala city, which was famous for its Pashupati Shivalinga. The name Nepal probably originates from this city Nayapala.
Very few historical records exists of the period before medieval Licchavi rulers. According to Gopalraj Vansawali, a genealogy of Nepali monarchy, the rulers of Kathmandu Valley before the Licchavis were Gopalas, Mahispalas, Aabhirs, Kiratas, and Somavanshi.[15][16] The Kirata dynasty was established by Yalamber. During the Kirata era, a settlement called Yambu existed in the northern half of old Kathmandu. In some of the Sino-Tibetan languages, Kathmandu is still called Yambu. Another smaller settlement called Yengal was present in the southern half of old Kathmandu, near Manjupattan. During the reign of the seventh Kirata ruler, Jitedasti, Buddhist monks entered Kathmandu valley and established a forest monastery at Sankhu.
Map of Kathmandu, 1802
Licchavi era
The Licchavis from the Indo-Gangetic plain migrated north and defeated the Kiratas, establishing the Licchavi dynasty, circa 400 AD. During this era, following the genocide of Shakyas in Lumbini by Virudhaka, the survivors migrated north and entered the forest monastery lora masquerading as Koliyas. From Sankhu, they migrated to Yambu and Yengal (Lanjagwal and Manjupattan) and established the first permanent Buddhist monasteries of Kathmandu. This created the basis of Newar Buddhism, which is the only surviving Sanskrit-based Buddhist tradition in the world.[17] With their migration, Yambu was called Koligram and Yengal was called Dakshin Koligram[18] during most of the Licchavi era.[19]
Eventually, the Licchavi ruler Gunakamadeva merged Koligram and Dakshin Koligram, founding the city of Kathmandu.[19] The city was designed in the shape of Chandrahrasa, the sword of Manjushri. The city was surrounded by eight barracks guarded by Ajimas. One of these barracks is still in use at Bhadrakali (in front of Singha Durbar). The city served as an important transit point in the trade between India and Tibet, leading to tremendous growth in architecture. Descriptions of buildings such as Managriha, Kailaskut Bhawan, and Bhadradiwas Bhawan have been found in the surviving journals of travellers and monks who lived during this era. For example, the famous 7th-century Chinese traveller Xuanzang described Kailaskut Bhawan, the palace of the Licchavi king Amshuverma.[20] The trade route also led to cultural exchange as well. The artistry of the Newar people—the indigenous inhabitants of the Kathmandu Valley—became highly sought after during this era, both within the Valley and throughout the greater Himalayas. Newar artists travelled extensively throughout Asia, creating religious art for their neighbours. For example, Araniko led a group of his compatriot artists through Tibet and China. Bhrikuti, the princess of Nepal who married Tibetan monarch Songtsän Gampo, was instrumental in introducing Buddhism to Tibet.
Skyline of Kathmandu, circa 1793
Malla era
The Licchavi era was followed by the Malla era. Rulers from Tirhut, upon being attacked by Muslims, fled north to the Kathmandu valley. They intermarried with Nepali royalty, and this led to the Malla era. The early years of the Malla era were turbulent, with raids and attacks from Khas and Turk Muslims. There was also a devastating earthquake which claimed the lives of a third of Kathmandu's population, including the king Abhaya Malla. These disasters led to the destruction of most of the architecture of the Licchavi era (such as Mangriha and Kailashkut Bhawan), and the loss of literature collected in various monasteries within the city. Despite the initial hardships, Kathmandu rose to prominence again and, during most of the Malla era, dominated the trade between India and Tibet. Nepali currency became the standard currency in trans-Himalayan trade.
During the later part of the Malla era, Kathmandu Valley comprised four fortified cities: Kantipur, Lalitpur, Bhaktapur, and Kirtipur. These served as the capitals of the Malla confederation of Nepal. These states competed with each other in the arts, architecture, esthetics, and trade, resulting in tremendous development. The kings of this period directly influenced or involved themselves in the construction of public buildings, squares, and temples, as well as the development of waterspouts, the institutionalisation of trusts (called guthis), the codification of laws, the writing of dramas, and the performance of plays in city squares. Evidence of an influx of ideas from India, Tibet, China, Persia, and Europe among other places can be found in a stone inscription from the time of king Pratap Malla. Books have been found from this era that describe their tantric tradition (e.g. Tantrakhyan), medicine (e.g. Haramekhala), religion (e.g. Mooldevshashidev), law, morals, and history. Amarkosh, a Sanskrit-Nepal Bhasa dictionary from 1381 AD, was also found. Architecturally notable buildings from this era include Kathmandu Durbar Square, Patan Durbar Square, Bhaktapur Durbar Square, the former durbar of Kirtipur, Nyatapola, Kumbheshwar, the Krishna temple, and others.
Medieval era
The Gorkha Kingdom ended the Malla confederation after the Battle of Kathmandu in 1768. This marked the beginning of the modern era in Kathmandu. The Battle of Kirtipur was the start of the Gorkha conquest of the Kathmandu Valley. Kathmandu was adopted as the capital of the Gorkha empire, and the empire itself was dubbed Nepal. During the early part of this era, Kathmandu maintained its distinctive culture. Buildings with characteristic Nepali architecture, such as the nine-story tower of Basantapur, were built during this era. However, trade declined because of continual war with neighbouring nations. Bhimsen Thapa supported France against Great Britain; this led to the development of modern military structures, such as modern barracks in Kathmandu. The nine-storey tower Dharahara was originally built during this era.
Rana rule
Rana rule over Nepal started with the Kot Massacre of 1846, which occurred near Hanuman Dhoka Durbar. During this massacre, most of Nepal's high-ranking officials were massacred by Jung Bahadur Rana and his supporters. Another massacre, the Bhandarkhal Massacre, was also conducted by Kunwar and his supporters in Kathmandu. During the Rana regime, Kathmandu's alliance shifted from anti-British to pro-British; this led to the construction of the first buildings in the style of Western European architecture. The most well-known of these buildings include Singha Durbar, Garden of Dreams, Shital Niwas, and the old Narayanhiti palace. The first modern commercial road in the Kathmandu Valley, the New Road, was also built during this era. Trichandra College (the first college of Nepal), Durbar High School (the first modern school of Nepal), and Bir Hospital (the first hospital of Nepal) were built in Kathmandu during this era. Education was only accessible to the privileged class. Rana rule was marked by despotism, economic exploitation and religious persecution.
Geography
Kathmandu is in the northwestern part of the Kathmandu Valley to the north of the Bagmati river and covers an area of 50.7 km2 (19.6 sq mi). The average elevation is 1,400 metres (4,600 ft) above sea level.[23] The city is bounded by several other municipalities of the Kathmandu valley: south of the Bagmati by Lalitpur Metropolitan City (Patan), with which it forms one urban area surrounded by a ring road, to the southwest by Kirtipur and to the east by Madyapur Thimi. To the north the urban area extends into several municipalities; Nagarjun, Tarakeshwor, Tokha, Budhanilkantha, Gokarneshwor and Kageshwori Manohara. However, the urban agglomeration extends well beyond the neighbouring municipalities, e.g. to Bhaktapur, and nearly covers the entire Kathmandu valley.
Kathmandu is dissected by eight rivers, the main river of the valley, the Bagmati and its tributaries, of which the Bishnumati, Dhobi Khola, Manohara Khola, Hanumante Khola, and Tukucha Khola are predominant. The mountains from where these rivers originate are in the elevation range of 1,500–3,000 metres (4,900–9,800 ft), and have passes which provide access to and from Kathmandu and its valley.[24][25][26] An ancient canal once flowed from Nagarjuna hill through Balaju to Kathmandu; this canal is now extinct.
The city of Kathmandu and the surrounding valley are in the Deciduous Monsoon Forest Zone (altitude range of 1,200–2,100 metres (3,900–6,900 ft)), one of five vegetation zones defined for Nepal. The dominant tree species in this zone are oak, elm, beech, maple and others, with coniferous trees at higher altitude.[27]
Urban expansion in Kathmandu, 2015.
The green, vegetated slopes that surround the Kathmandu metro area (light grey, image centre) include both forest reserves and national parks
Araniko Highway connects Kathmandu to Bhaktapur and onwards to the Chinese border.
Northeastern Kathmandu with Gaurishankar in background.
Kathmandu administration
Kathmandu and adjacent cities are composed of neighbourhoods, which are utilized quite extensively and more familiar among locals. However, administratively the city is divided into 32 wards, numbered from 1 to 32. Earlier, there were 35 wards which made it the metropolitan city with the largest number of the wards.[28]
Kathmandu agglomeration
There is no officially defined agglomeration of Kathmandu. The urban area of the Kathmandu valley is split among three different districts (second level of administrative divisions within a province), which extend very little beyond the valley fringe, except towards the southern ranges, which have a comparatively small population.[29] They have the three highest population densities in the country. These 3 districts are administered by 21 local level bodies; 2 metropolitan cities (Kathmandu and Lalitpur), 16 municipalities and 3 rural municipalities. Imperial conversion
Five major climatic regions are found in Nepal. Of these, Kathmandu Valley is in the Warm Temperate Zone (elevation ranging from 1,200 to 2,300 metres (3,900 to 7,500 ft)), where the climate is fairly temperate, atypical for the region. This zone is followed by the Cool Temperate Zone with elevation varying between 2,100 and 3,300 metres (6,900 and 10,800 ft). Under Köppen's climate classification, portions of the city with lower elevations have a humid subtropical climate (Cwa), while portions of the city with higher elevations generally have a subtropical highland climate (Cwb). In the Kathmandu Valley, which is representative of its valley's climate, the average summer temperature varies from 28 to 30 °C (82 to 86 °F). The average winter temperature is 10.1 °C (50.2 °F).
The city generally has a climate with warm days followed by cool nights and mornings. Unpredictable weather is expected, given that temperatures can drop to 1 °C (34 °F) or less during the winter. During a 2013 cold front, the winter temperatures of Kathmandu dropped to −4 °C (25 °F), and the lowest temperature was recorded on 10 January 2013, at −9.2 °C (15.4 °F). Rainfall is mostly monsoon-based (about 65% of the total concentrated during the monsoon months of June to September), and decreases substantially (100 to 200 cm (39 to 79 in)) from eastern Nepal to western Nepal. Rainfall has been recorded at about 1,400 millimetres (55.1 in) for the Kathmandu valley, and averages 1,407 millimetres (55.4 in) for the city of Kathmandu. On average humidity is 75%.[24][30][31] The chart below is based on data from the Nepal Bureau of Standards & Meteorology, Weather Meteorology for 2005. The chart provides minimum and maximum temperatures during each month. The annual amount of precipitation was 1,124 millimetres (44.3 in) for 2005, as per monthly data included in the table above.[31] The decade of 2000–2010 saw highly variable and unprecedented precipitation anomalies in Kathmandu. This was mostly due to the annual variation of the southwest monsoon.[citation needed] For example, 2001 recorded only 356 mm (14 in) of precipitation due to an extraordinarily weak monsoon season. In contrast, 2003 was the wettest year ever in Kathmandu, totaling over 2,900 mm (114 in) of precipitation due to an exceptionally strong monsoon season.
Air quality
Air pollution is a major issue in the Kathmandu Valley.[36][37][38] According to the 2016 World Health Organization's Ambient Air Pollution Database,[39] the annual average PM2.5 (particulate matter) concentration in 2013 was 49 μg/m3, which is 4.9 times higher than recommended by the World Health Organization.[40][41] Starting in early 2017, the Government of Nepal and the Embassy of the United States in Kathmandu have monitored and publicly share real-time air quality data. In Nepal and Kathmandu, the annual premature deaths due to air pollution reached 37,399 and 9,943 respectively, according to a Republica news report published on 23 November, 2019. This indicates, around a quarter of the total deaths due to air pollution in Nepal are in Kathmandu.
Government and public services
Kathmandu Municipal Corporation (KMC) is the chief nodal agency for the administration of Kathmandu. The Municipality of Kathmandu was upgraded to a metropolitan city in 1995.
Metropolitan Kathmandu is divided into five sectors: the Central Sector, the East Sector, the North Sector, the City Core and the West Sector. For civic administration, the city is further divided into 35 administrative wards. The Council administers the Metropolitan area of Kathmandu city through its 177 elected representatives and 20 nominated members. It holds biannual meetings to review, process and approve the annual budget and make major policy decisions.[24][44] The ward's profile documents for the 35 wards prepared by the Kathmandu Metropolitan Council is detailed and provides information for each ward on population, the structure and condition of houses, the type of roads, educational, health and financial institutions, entertainment facilities, parking space, security provisions, etc. It also includes lists of development projects completed, on-going and planned, along with informative data about the cultural heritage, festivals, historical sites and the local inhabitants. Ward 16 is the largest, with an area of 437.4 ha; ward 26 is the smallest, with an area of 4 ha.[45]
Kathmandu is the headquarters of the surrounding Kathmandu district. The city of Kathmandu forms this district along with 10 other municipalities, namely Budanilkantha, Chandragiri, Dakshinkali, Gokarneshwar, Kageshwari Manohara, Kirtipur, Nagarjun, Shankharapur, Tarakeshwar and Tokha.
Law and order
The Metropolitan Police is the main law enforcement agency in the city. It is headed by a commissioner of police. The Metropolitan Police is a division of the Nepal Police, and the administrative control lies with the Ministry of Home Affairs.
Consulate of the Netherlands. Kathmandu hosts 28 diplomatic missions
Fire service
The fire service, known as the Barun Yantra Karyalaya (Nepali: वारुण यन्त्र कार्यालय), opened its first station in Kathmandu in 1937 with a single-vehicle.[46] An iron tower was erected to monitor the city and watch for a fire. As a precautionary measure, firemen were sent to the areas which were designated as accident-prone areas.[46] In 1944, the fire service was extended to the neighbouring cities of Lalitpur and Bhaktapur. In 1966, a fire service was established in Kathmandu central airport.[46] In 1975, a West German government donation added seven fire engines to Kathmandu's fire service.[46] The fire service in the city is also overlooked by an international non-governmental organization, the Firefighters Volunteer Association of Nepal (FAN), which was established in 2000 with the purpose of raising public awareness about fire and improving safety.[46]
Electricity and water supply
Public baths, Kathmandu. 1979
Electricity in Kathmandu is regulated and distributed by the Nepal Electricity Authority (NEA). Water supply and sanitation facilities are provided by the Kathmandu Upatyaka Khanepani Limited (KUKL). There is a severe shortage of water for household purposes such as drinking, bathing, cooking and washing and irrigation. People have been using bottled mineral water, water from tank trucks and from the ancient dhunge dharas (Nepali: ढुङ्गे धारा) for all the purposes related to water. The city water shortage should be solved by the completion of the much plagued Melamchi Water Supply Project by the end of 2019.[47][48]
Waste management
Waste management may be through composting in municipal waste management units, and at houses with home composting units. Both systems are common and established in India and neighbouring countries.[49]
Demographics
Kathmandu's urban cosmopolitan character has made it the most populous city in Nepal, recording a population of 671,846 residents living in 235,387 households in the metropolitan area, according to the 2001 census.[50] According to the National Population Census of 2011, the total population of Kathmandu city was 975,543 with an annual growth rate of 6.12% with respect to the population figure of 2001. 70% of the total population residing in Kathmandu are aged between 15 and 59.
Over the years the city has been home to people of various ethnicities, resulting in a range of different traditions and cultural practices. In one decade, the population increased from 427,045 in 1991 to 671,805 in 2001. The population was projected to reach 915,071 in 2011 and 1,319,597 by 2021. To keep up this population growth, the KMC-controlled area of 5,076.6 hectares (12,545 acres) has expanded to 8,214 hectares (20,300 acres) in 2001. With this new area, the population density which was 85 in 1991 remained 85 in 2001; it is likely to jump to 111 in 2011 and 161 in 2021.[51]
Currently based on various data Kathmandu population is 1,442,300 with population density of 29,166.835 per sq.km making it as 6th densely populated city in the world.
Ethnic groups
The largest ethnic groups residing in Kathmandu Metropolitan City consists of primarily various caste groups of the Newar community at 25%, Hill Janajati/Adivisis like Tamang, Kirat, Gurung, Magar, Sherpa, etc. making~20%, Khas Brahmin at 24%, Khas Chhetri at 20%, and 7% Terai groups including Madhesi castes and Terai Janajatis/Adivasis like Tharus.[52] More recently, other hill ethnic groups and caste groups from Terai have come to represent a substantial proportion of the city's population. The major languages are Nepali and Nepal Bhasa, while English is understood by many, particularly in the service industry. According to data from 2011, the major religions in Kathmandu city are Hinduism 81.3%, Buddhism 9%, Islam 4.4% and other 5.2%.[53]
The linguistic profile of Kathmandu underwent drastic changes during the Shah dynasty's rule because of its strong bias towards the Hindu culture. Sanskrit language therefore was preferred and people were encouraged to learn it even by attending Sanskrit learning centres in Terai. Sanskrit schools were specially set up in Kathmandu and in the Terai region to inculcate traditional Hindu culture and practices originated from Nepal.[54]
Architecture and cityscape
The ancient trade route between India and Tibet that passed through Kathmandu enabled a fusion of artistic and architectural traditions from other cultures to be amalgamated with local art and architecture.[56] The monuments of Kathmandu City have been influenced over the centuries by Hindu and Buddhist religious practices. The architectural treasure of the Kathmandu valley has been categorized under the well-known seven groups of heritage monuments and buildings. In 2006 UNESCO declared these seven groups of monuments as a World Heritage Site (WHS). The seven monuments zones cover an area of 189 hectares (470 acres), with the buffer zone extending to 2,394 hectares (5,920 acres). The Seven Monument Zones inscribed originally in 1979 and with a minor modification in 2006 are the Durbar squares of Hanuman Dhoka, Patan and Bhaktapur, the Hindu temples of Pashupatinath and Changunarayan, the Buddhist stupas of Swayambhunath and Boudhanath.[57][58]
Durbar Squares
Main articles: Kathmandu Durbar Square and Hanuman Dhoka
The literal meaning of Durbar Square is a "place of palaces." There are three preserved Durbar Squares in Kathmandu valley and one unpreserved in Kirtipur. The Durbar Square of Kathmandu is in the old city and has heritage buildings representing four kingdoms (Kantipur, Lalitpur, Bhaktapur, Kirtipur); the earliest being the Licchavi dynasty. The complex has 50 temples and is distributed in two quadrangles of the Durbar Square. The outer quadrangle has the Kasthamandap, Kumari Ghar, and Shiva-Parvati Temple; the inner quadrangle has the Hanuman Dhoka palace. The squares were severely damaged in the April 2015 earthquake.
Hanuman Dhoka is a complex of structures with the royal palace of the Malla kings and of the Shah dynasty. It is spread over five acres. The eastern wing, with ten courtyards, is the oldest part, dating to the mid-16th century. It was expanded by King Pratap Malla in the 17th century with many temples. The royal family lived in this palace until 1886 when they moved to Narayanhiti Palace. The stone inscription outside is in fifteen languages.
Kumari Ghar is a palace in the centre of the Kathmandu city, next to the Durbar square where a royal Kumari selected from several Kumaris resides. Kumari, or Kumari Devi, is the tradition of worshipping young pre-pubescent girls as manifestations of the divine female energy or devi in South Asian countries. In Nepal the selection process is very rigorous. Previously, during the time of the monarchy, the queen and the priests used to appoint the proposed Kumari with delicate process of astrological examination and physical examination of 32 'gunas'. The china (Nepali: चिना), an ancient Hindu astrological report, of the Kumari and the reigning king, was ought to be similar. The Kumari is believed to be a bodily incarnation of the goddess Taleju (the Nepali name for Durga) until she menstruates, after which it is believed that the goddess vacates her body. Serious illness or a major loss of blood from an injury also causes her to revert to common status. The current Kumari, Trishna Shakya, age three at the time of appointment, was installed in September 2017 succeeding Matina Shakya who was the first Kumari of Kathmandu after the end of the monarchy.[59]
Kasthamandap is a three-storeyed temple enshrining an image of Gorakhnath. It was built in the 16th century in pagoda style. The name of Kathmandu is a derivative of the word Kasthamandap. It was built under the reign of King Laxmi Narsingha Malla. Kasthamandap stands at the intersection of two ancient trade routes linking India and Tibet at Maru square. It was originally built as a rest house for travellers.
Pashupatinath temple
Main article: Pashupatinath Temple
Panorama of the Pashupatinath Temple from the other bank of Bagmati river
Pashupatinath as seen from the banks of the Bagmati river
The Pashupatinath Temple (Nepali: पशुपतिनाथ मन्दिर) is a famous 5th century Hindu temple dedicated to Lord Shiva. Located on the banks of the Bagmati river, the Pashupatinath Temple is the oldest Hindu temple in Kathmandu.[60] It served as the seat of national deity, Lord Pashupatinath, until Nepal was secularized. However, a significant part of the temple was destroyed by Mughal invaders in the 14th century and little or nothing remains of the original 5th-century temple exterior. The temple as it stands today was built in the 19th century, although the image of the bull and the black four-headed image of Pashupati are at least 300 years old.[61] The temple is a UNESCO World Heritage Site.[61][62] Shivaratri, or the night of Lord Shiva, is the most important festival that takes place here, attracting thousands of devotees and sadhus.[citation needed]
Believers in Pashupatinath (mainly Hindus) are allowed to enter the temple premises, but non-Hindu visitors are allowed to view the temple only from the across the Bagmati River.[61] The priests who perform the services at this temple have been Brahmins from Karnataka in southern India since the time of Malla king Yaksha Malla.[63] This tradition is believed to have been started at the request of Adi Shankaracharya who sought to unify the states of Bharatam, a region in south Asia believed to be ruled by a mythological king Bharat, by encouraging cultural exchange. This procedure is followed in other temples around India, which were sanctified by Adi Shankaracharya.
The temple is built in the pagoda style of architecture, with cubic constructions and carved wooden rafters (tundal) on which they rest, and two-level roofs made of copper and gold.
Boudhanath
Boudhanath (Nepali: बौद्ध स्तुप; also written as Bouddhanath, Bodhnath, Baudhanath or the Khāsa Chaitya), is one of the holiest Buddhist sites in Nepal, along with the Swayambhunath. It is a very popular tourist site. Boudhanath is known as Khāsti by Newars and as Bauddha or Bodhnāth by speakers of Nepali.[64] About 11 km (7 mi) from the centre and northeastern outskirts of Kathmandu, the stupa's massive mandala makes it one of the largest spherical stupas in Nepal.[65] Boudhanath became a UNESCO World Heritage Site in 1979.
The base of the stupa has 108 small depictions of the Dhyani Buddha Amitabha. It is surrounded with a brick wall with 147 niches, each with four or five prayer wheels engraved with the mantra, om mani padme hum.[66] At the northern entrance where visitors must pass is a shrine dedicated to Ajima, the goddess of smallpox.[66] Every year the stupa attracts many Tibetan Buddhist pilgrims who perform full body prostrations in the inner lower enclosure, walk around the stupa with prayer wheels, chant, and pray.[66] Thousands of prayer flags are hoisted up from the top of the stupa downwards and dot the perimeter of the complex. The influx of many Tibetan refugees from China has seen the construction of over 50 Tibetan gompas (monasteries) around Boudhanath.
Swayambhu
Main article: Swayambhunath
Swayambhunath (Nepali: स्वयम्भू स्तूप) is a Buddhist stupa atop a hillock at the northwestern part of the city. This is among the oldest religious sites in Nepal. Although the site is considered Buddhist, it is revered by both Buddhists and Hindus. The stupa consists of a dome at the base; above the dome, there is a cubic structure with the eyes of Buddha looking in all four directions.[clarification needed] There are pentagonal toran above each of the four sides, with statues engraved on them. Behind and above the torana there are thirteen tiers. Above all the tiers, there is a small space above which lies a gajur.
Rani Pokhari
Main article: Ranipokhari
Ranipokhari (Nepali: रानी पोखरी, lit. 'Queen's Pond') is a historic artificial pond nestled in the heart of Kathmandu. It was built by king Pratap Malla in 1670 AD for his beloved queen after she lost her son and could not recover from her loss.[67] A large stone statue of an elephant in the south signifies the image of Pratap Malla and his two sons. Balgopaleshwor Temple stands still inside the temple above the pond. Rani Pokhari is opened once a year during the final day of Tihar i.e. Bhai Tika and Chhath festival. The world's largest Chhath takes place every year in Ranipokhari. The pond is one of Kathmandu's most famous landmarks and is known for its religious and aesthetic significance.
Culture
Main article: Culture of Kathmandu
Arts
Stone carvings, called Chaityas, seen in street corners and courtyards
Kathmandu valley is described as "an enormous treasure house of art and sculptures", which are made of wood, stone, metal, and terracotta, and found in profusion in temples, shrines, stupas, gompas, chaityasm and palaces. The art objects are also seen in street corners, lanes, private courtyards and in open ground. Most art is in the form of icons of gods and goddesses. Kathmandu valley has had this art treasure for a very long time, but received worldwide recognition only after the country opened to the outside world in 1950.[54]
The religious art of Nepal and Kathmandu in particular consists of an iconic symbolism of the Mother Goddesses such as: Bhavani, Durga, Gaja-Lakshmi, Hariti-Sitala, Mahsishamardini, Saptamatrika (seven mother goddesses), and Sri-Lakshmi (wealth-goddess). From the 3rd century BCE, apart from the Hindu gods and goddesses, Buddhist monuments from the Ashokan period (it is said that Ashoka visited Nepal in 250 BC) have embellished Nepal in general and the valley in particular. These art and architectural edifices encompass three major periods of evolution: the Licchavi or classical period (500 to 900 AD), the post-classical period (1000 to 1400 AD), with strong influence of the Palla art form; the Malla period (1400 onwards) that exhibited explicitly tantric influences coupled with the art of Tibetan Demonology.[68]
A broad typology has been ascribed to the decorative designs and carvings created by the people of Nepal. These artists have maintained a blend of Hinduism and Buddhism. The typology, based on the type of material used are: stone art, metal art, wood art, terracotta art, and painting.[69]
Museums
Kathmandu is home to a number of museums and art galleries, including the National Museum of Nepal and the Natural History Museum of Nepal. Nepal's art and architecture is an amalgamation of two ancient religions, Hinduism and Buddhism. These are amply reflected in the many temples, shrines, stupas, monasteries, and palaces in the seven well-defined Monument Zones of the Kathmandu valley are part of a UNESCO World Heritage Site. This amalgamation is also reflected in the planning and exhibitions in museums and art galleries throughout Kathmandu and its sister cities of Patan and Bhaktapur. The museums display unique artefacts and paintings from the 5th century CE to the present day, including archaeological exportation.[70]
Museums and art galleries in Kathmandu include:[70]
The National Museum
The Natural History Museum
Hanuman Dhoka Palace Complex
The Kaiser Library
The National Art Gallery
The NEF-ART (Nepal Fine Art) Gallery
The Nepal Art Council Gallery
Narayanhiti Palace Museum
The Taragaon Museum
National Museum of Nepal
The National Museum is in the western part of Kathmandu, near the Swayambhunath stupa in a historical building constructed in the early 19th century by General Bhimsen Thapa. It is the most important museum in the country, housing an extensive collection of weapons, art and antiquities of historic and cultural importance. The museum was established in 1928 as a collection house of war trophies and weapons, and the initial name of this museum was Chhauni Silkhana, meaning "the stone house of arms and ammunition". Given its focus, the museum contains many weapons, including locally made firearms used in wars, leather cannons from the 18th–19th century, and medieval and modern works in wood, bronze, stone and paintings.[71]
The Natural History Museum is in the southern foothills of Swayambhunath hill and has a sizeable collection of different species of animals, butterflies, and plants. The museum is noted for its display of species, from prehistoric shells to stuffed animals.[71]
The Tribhuvan Museum contains artifacts related to King Tribhuvan (1906–1955). It has a variety of pieces including his personal belongings, letters, and papers, memorabilia related to events he was involved in and a rare collection of photos and paintings of Royal family members. The Mahendra Museum is dedicated to the King Mahendra (1920–1972). Like the Tribhuvan Museum, it includes his personal belongings such as decorations, stamps, coins and personal notes and manuscripts, but it also has structural reconstructions of his cabinet room and office chamber. The Hanumandhoka Palace, a lavish medieval palace complex in the Durbar, contains three separate museums of historic importance. These museums include the Birendra museum, which contains items related to the second-last monarch, King Birendra.[71]
The enclosed compound of the Narayanhiti Palace Museum is in the north-central part of Kathmandu. "Narayanhiti" (Nepali: नारायणहिटी) comes from Narayana (Nepali: नारायण), a form of the Hindu god Lord Vishnu, and Hiti (Nepali: हिटी), meaning "water spout" (the temple of lord Vishnu is opposite to the palace, and the water spout is east of the main entrance to the precinct). The current palace building was built in 1970 in front of the old palace, built in 1915, in the form of a contemporary pagoda. It was built on the occasion of the marriage of the then crown prince and heir apparent to the throne, Birendra. The southern gate of the palace is at the crossing of Prithvipath and Durbar Marg roads. The palace area covers 30 hectares (74 acres) and is fully secured with gates on all sides.[72][73][74] This palace was the scene of the Nepali royal massacre. After the fall of the monarchy, it has been converted into a museum.
The Taragaon Museum presents the modern history of the Kathmandu valley.[75] It seeks to document 50 years of research and cultural heritage conservation of the Kathmandu Valley, documenting what artists, photographers, architects, and anthropologists from abroad had contributed in the second half of the 20th century. The actual structure of the museum showcases restoration and rehabilitation efforts to preserve the built heritage of Kathmandu. It was designed by Carl Pruscha (master-planner of the Kathmandu Valley)[76] in 1970 and constructed in 1971.[77] Restoration works began in 2010 to rehabilitate the Taragaon hostel into the Taragaon Museum. The design uses local brick along with modern architectural design elements, as well as the use of circle, triangles and squares.[76] The museum is within a short walk from the Boudhanath stupa, which itself can be seen from the museum tower.
Art galleries
A Buddhist statue display in Kathmandu
Kathmandu is a centre for art in Nepal, displaying the work of contemporary artists in the country and also collections of historical artists. Patan in particular is an ancient city noted for its fine arts and crafts. Art in Kathmandu is vibrant, demonstrating a fusion of traditionalism and modern art, derived from a great number of national, Asian, and global influences. Nepali art is commonly divided into two areas: the idealistic traditional painting known as Paubhas in Nepal and perhaps more commonly known as Thangkas in Tibet, closely linked to the country's religious history and on the other hand the contemporary western-style painting, including nature-based compositions or abstract artwork based on Tantric elements and social themes of which painters in Nepal are well noted for.[71] Internationally, the British-based charity, the Kathmandu Contemporary Art Centre is involved with promoting arts in Kathmandu.[78]
Kathmandu houses many notable art galleries. The NAFA Gallery, operated by the Arts and crafts Department of the Nepal Academy is housed in Sita Bhavan, a neo-classical old Rana palace.[71]
The Srijana Contemporary Art Gallery, inside the Bhrikutimandap Exhibition grounds, hosts the work of contemporary painters and sculptors, and regularly organizes exhibitions. It also runs morning and evening classes in the schools of art. Also of note is the Moti Azima Gallery, in a three-storied building in Bhimsenthan which contains an impressive collection of traditional utensils and handmade dolls and items typical of a medieval Newar house, giving an important insight into Nepali history. The J Art Gallery near the former royal palace in Durbarmarg displays the artwork of eminent, established Nepali painters. The Nepal Art Council Gallery, in the Babar Mahal, on the way to Tribhuvan International Airport contains artwork of both national and international artists and extensive halls regularly used for art exhibitions.[71]
Literature
The National Library of Nepal is located in Patan. It is the largest library in the country with more than 70,000 books in English, Nepali, Sanskrit, Hindi, and Nepal Bhasa. The library is in possession of rare scholarly books in Sanskrit and English dating from the 17th century AD. Kathmandu also contains the Kaiser Library, in the Kaiser Mahal on the ground floor of the Ministry of Education building. This collection of around 45,000 books is derived from a personal collection of Kaiser Shamsher Jang Bahadur Rana. It covers a wide range of subjects including history, law, art, religion, and philosophy, as well as a Sanskrit manual of Tantra, which is believed to be over 1,000 years old.[71] The 2015 earthquake caused severe damage to the Ministry of Education building, and the contents of the Kaiser Library have been temporarily relocated.
Asa Archives
The Asa Archives are also noteworthy. They specialize in medieval history and religious traditions of the Kathmandu valley. The archives, in Kulambhulu, have a collection of some 6,000 loose-leaf handwritten books and 1,000 palm-leaf manuscripts (mostly in Sanskrit or Nepal Bhasa) and a manuscript dated to 1464.[71]
Cinema and theatre
Kathmandu is home to Nepali cinema and theatres. The city contains several theatres, including the National Dance Theatre in Kanti Path, the Ganga Theatre, the Himalayan Theatre and the Aarohan Theater Group founded in 1982. The M. Art Theater is based in the city. The Gurukul School of Theatre organizes the Kathmandu International Theater Festival, attracting artists from all over the world.[79] A mini theatre has been opened at the Hanumandhoka Durbar Square, established by the Durbar Conservation and Promotion Committee.
Kathmandu has a number of cinemas (old single screen establishments and some new multiplexes) showing Nepali, Bollywood and Hollywood films. Some old establishments include Vishwajyoti Cinema Hall, Jai Nepal Hall, Kumari Cinema Hall, Gopi Krishna Cinema Hall and Guna Cinema Hall. Kathmandu also houses some international standard cinema theatres and multiplexes, such as QFX Cinemas, Cine De Chef, Fcube Cinemas, Q's Cinemas, Big Movies, BSR Movies and many more.
Music
Traditional Buddhist musical performance during Gunla
Kathmandu is the center of music and dance in Nepal, and these art forms are integral to understanding the city. Musical performances are organized in cultural venues. Music is a part of the traditional aspect of Kathmandu. Gunla is the traditional music festival according to Nepal Sambat. Newar music originated in Kathmandu. Furthermore, music from all over Nepal can be found in Kathmandu.
A number of hippies visited Kathmandu during the 1970s and introduced rock and roll, rock, and jazz to the city. Kathmandu is noted internationally for its jazz festival, popularly known as Jazzmandu. It is the only jazz festival in the Himalayan region and was established in March 2002. The festival attracts musicians from countries worldwide, such as Australia, Denmark, United States, Benin, and India.[80]
The city has been referenced in numerous songs, including works by Cat Stevens ('Katmandu', Mona Bone Jakon (1970)), Bob Seger ('Katmandu', Beautiful Loser (1975)), Rush ('A Passage to Bangkok', Pulling into Kathmandu; 2112, 1976), Krematorij ('Kathmandu', Three Springs (2000)), Fito Páez (Tráfico por Katmandú – "Traffic through Kathmandu") and Cavalcade ('Kathmandu Kid') 2019.
Cuisine
One of the typical Nepali meals Dal bhat in Kathmandu
The staple food of most people in Kathmandu is dal bhat. This consists of rice and lentil soup, generally served with vegetable curries, achar and sometimes Chutney. Momo, a type of Nepali version of Tibetan dumpling, has become prominent in Nepal with many street vendors and restaurants selling it. It is one of the most popular fast foods in Kathmandu. Various Nepali variants of momo including buff (i.e. buffalo) momo, chicken momo, and vegetarian momo are famous in Kathmandu.
Most of the cuisines found in Kathmandu are non-vegetarian. However, the practice of vegetarianism is not uncommon, and vegetarian cuisines can be found throughout the city. Consumption of beef is very uncommon and considered taboo in many places. Buff (meat of water buffalo) is very common. There is a strong tradition of buff consumption in Kathmandu, especially among Newars, which is not found in other parts of Nepal. Consumption of pork was considered taboo until a few decades ago. Due to the intermixing with Kirat cuisine from eastern Nepal, pork has found a place in Kathmandu dishes. A fringe population of devout Hindus and Muslims consider it taboo. The Muslims forbid eating buff as from Quran while Hindus eat all varieties except beef as they consider cow to be a goddess and symbol of purity. The chief lunch/snack for locals and visitors is mostly Momo or Chowmein.
Kathmandu had only one western-style restaurant in 1955.[81] A large number of restaurants in Kathmandu have since opened, catering Nepali cuisine, Tibetan cuisine, Chinese cuisine and Indian cuisine in particular. Many other restaurants have opened to accommodate locals, expatriates, and tourists. The growth of tourism in Kathmandu has led to culinary creativity and the development of hybrid foods to accommodate for tourists such as American chop suey, which is a sweet-and-sour sauce with crispy noodles with a fried egg commonly added on top and other westernized adaptations of traditional cuisine.[81] Continental cuisine can be found in selected places. International chain restaurants are rare, but some outlets of Pizza Hut and KFC have recently opened there. It also has several outlets of the international ice-cream chain Baskin-Robbins.[82]
Kathmandu has a larger proportion of tea drinkers than coffee drinkers. Tea is widely served but is extremely weak by western standards. It is richer and contains tea leaves boiled with milk, sugar, and spices. Alcohol is widely drunk, and there are numerous local variants of alcoholic beverages. Drinking and driving is illegal, and authorities have a zero-tolerance policy.[83] Ailaa and thwon (alcohol made from rice) are the alcoholic beverages of Kathmandu, found in all the local bhattis (alcohol serving eateries). Chhyaang, tongba (fermented millet or barley) and raksi are alcoholic beverages from other parts of Nepal which are found in Kathmandu. However, shops and bars in Kathmandu widely sell western and Nepali beers.
President of Nepal Dr. Ram Baran Yadav observing the street festival of Yenya, which literally means "festival of Kathmandu"
Festivals
Samyak, a Buddhist festival during which statues of Buddhas from the ancient monasteries are displayed together. Note the statue of Hanuman next to the Buddhas in the picture, a common example of religious harmony in Kathmandu.
Most of the fairs and festivals in Kathmandu originated in the Malla period or earlier. Traditionally, these festivals were celebrated by Newars. In recent years, these festivals have found wider participation from other Kathmanduites as well. As the capital of the Nepal, various national festivals are celebrated in Kathmandu. With mass migration to the city, the cultures of Khas from the west, Kirats from the east, Bon/Tibetan from the north, and Mithila from the south meet in the capital and mingle harmoniously. The festivities such as the Ghode (horse) Jatra, Indra Jatra, Dashain Durga Puja festivals, Shivratri and many more are observed by all Hindu and Buddhist communities of Kathmandu with devotional fervor and enthusiasm. Social regulation in the codes enacted incorporates Hindu traditions and ethics. These were followed by the Shah kings and previous kings, as devout Hindus and protectors of the Buddhist religion.
Nepali Lakhe dancer
Cultural continuity has been maintained for centuries in the exclusive worship of goddesses and deities in Kathmandu and the rest of the country. These deities include the Ajima,[84] Taleju (or Tulja Bhavani or Taleju Bhawani)[85][86] and her other forms : Digu Taleju (or Degu Taleju)[87] and Kumari (the living goddess).[88] The artistic edifices have now become places of worship in the everyday life of the people, therefore a roster is maintained to observe annual festivals. There are 133 festivals held in the year.[89]
Some of the traditional festivals observed in Kathmandu, apart from those previously mentioned, are Bada Dashain, Tihar, Chhath, Maghe Sankranti, Nag Panchami, Janai Purnima, Pancha Dan, Teej/Rishi Panchami, Pahan Charhe, Jana Baha Dyah Jatra (White Machchhendranath Jatra), and Matatirtha Aunsi.[56]
Religions
Hinduism
Kathmandu valley as seen from Halchowk during Deepawali, 2013
Assumedly, together with the kingdom of Licchhavi (c. 400 to 750), Hinduism and the endogam social stratification of the caste was established in Kathmandu Valley. The Pashupatinath Temple, Changu Narayan Temple, and the Kasthamandap are of particular importance to Hindus. Other notable Hindu temples in Kathmandu and the surrounding valley include Bajrayogini Temple, Dakshinkali Temple, Guhyeshwari Temple, and the Shobha Bhagawati shrine.
The Bagmati river which flows through Kathmandu is considered a holy river both by Hindus and Buddhists, and many Hindu temples are on the banks of this river. The importance of the Bagmati also lies in the fact that Hindus are cremated on its banks, and Kirants are buried in the hills by its side. According to the Nepali Hindu tradition, the dead body must be dipped three times into the Bagmati before cremation. The chief mourner (usually the first son) who lights the funeral pyre must take a holy riverwater bath immediately after cremation. Many relatives who join the funeral procession also take bath in the Bagmati or sprinkle the holy water on their bodies at the end of cremation as the Bagmati is believed to purify people spiritually.
Buddhism
Buddhism was brought into Kathmandu with the arrival of Buddhist monks during the time of Buddha (c. 563 – 483 BCE[90]). They established a forest monastery in Sankhu. This monastery was renovated by Shakyas after they fled genocide from Virudhaka (r. 491–461 BCE).
During the Hindu Lichchavi era (c. 400 to 750), various monasteries and orders were created which successively led to the formation of Newar Buddhism, which is still practiced in the primary liturgical language of Hinduism, Sanskrit.
Legendary Princess Bhrikuti (7th-century) and artist Araniko (1245–1306 CE) from that tradition of Kathmandu valley played a significant role in spreading Buddhism in Tibet and China. There are over 108 traditional monasteries (Bahals and Baháʼís) in Kathmandu based on Newar Buddhism. Since the 1960s, the permanent Tibetan Buddhist population of Kathmandu has risen significantly so that there are now over fifty Tibetan Buddhist monasteries in the area. Also, with the modernization of Newar Buddhism, various Theravada Bihars have been established.
Islam
Jama Masjid, Ghantaghar
Muslims in Kathmandu pray to Allah on Friday (the day of Namaj) often going to the Jame Masjid in Ghantaghar, near Ratnapark.
Kirat Mundhum
Kirant Mundhum is one of the indigenous animistic practices of Nepal. It is practiced by the Kirat people. Some animistic aspects of Kirant beliefs, such as ancestor worship (worship of Ajima) are also found in Newars of Kirant origin. Ancient religious sites believed to be worshipped by ancient Kirats, such as Pashupatinath, Wanga Akash Bhairabh (Yalambar) and Ajima are now worshipped by people of all Dharmic religions in Kathmandu. Kirats who have migrated from other parts of Nepal to Kathmandu practice Mundhum in the city.[91]
Other religions
Sikhism is practiced primarily in Gurudwara at Kupundole. An earlier temple of Sikhism is also present in Kathmandu which is now defunct.
Jainism is practiced by a small community. A Jain temple is present in Gyaneshwar, where Jains practice their faith.
According to the records of the Spiritual Assembly of the Baháʼís of Nepal, there are approximately 300 followers of the Baháʼí Faith in Kathmandu valley. They have a national office in Shantinagar, Baneshwor. The Baháʼís also have classes for children at the National Centre and other localities in Kathmandu.
Islam is practiced in Kathmandu but Muslims are a minority, accounting for about 4.4% of the population of Nepal.[92]
It is said that in Kathmandu alone there are 170 Christian churches. Christian missionary hospitals, welfare organizations, and schools are also operating. Nepali citizens who served as soldiers in Indian and British armies, who had converted to Christianity while in service, on return to Nepal continue to practice their religion. They have contributed to the spread of Christianity and the building of churches in Nepal and in Kathmandu, in particular.[93][94]
Education
The oldest modern school in Nepal, the Durbar High School, and the oldest college, the Tri-Chandra College, are both in Kathmandu. The largest (according to number of students and colleges), the oldest and most distinguished university in Nepal the Tribhuvan University, located in Kirtipur. The second largest university, Kathmandu University (KU), is in Dhulikhel, Kavre on the outskirts of Kathmandu. It is the second oldest university in Nepal, established in November 1991.[95] Not surprisingly the best schools and colleges of Nepal are located in Kathmandu and its adjoining cities. Every year thousands of students from all over Nepal arrive at Kathmandu to get admission in the various schools and colleges. One of the key concerns of educationists and concerned citizens is the massive outflux of students from Nepal to outside Nepal for studies. Every year thousands of students apply for No Objection Certificates for studying abroad. Consultancy firms specializing in preparing students to go abroad can be found in all prominent locations. The reason for such an outflux range from perceived low quality of education, political instability, fewer opportunities in the job market, opportunities for earning while learning abroad and better job prospects with an international degree.
Healthcare
Healthcare in Kathmandu is the most developed in Nepal, and the city and surrounding valley is home to some of the best hospitals and clinics in the country. Bir Hospital is the oldest, established in July 1889 by Bir Shamsher Jang Bahadur Rana. Notable hospitals include Bir Hospital, Nepal Medical College and Teaching Hospital (Jorpati), Tribhuvan University Institute of Medicine (Teaching Hospital), Patan Hospital, Kathmandu Model Hospital, Scheer Memorial Hospital, Om Hospital, Norvic Hospital, Grande International Hospital, Nobel Hospital and many more.
The city is supported by specialist hospitals/clinics such as Shahid Shukraraj Tropical Hospital, Shahid Gangalal Foundation, Kathmandu Veterinary Hospital, Nepal Eye Hospital, Kanti Children's Hospital, Nepal International Clinic (Travel and Mountain Medicine Center), Neuro Center, Spinal Rehabilitation center and Bhaktapur Cancer Hospital. Most of the general hospitals are in the city center, although several clinics are elsewhere in Kathmandu district.
Tilganga Institute of Ophthalmology is an Ophthalmological hospital in Kathmandu. It pioneered the production of low cost intraocular lenses (IOLs), which are used in cataract surgery.[96] The team of Dr. Sanduk Ruit in Tilganga pioneered sutureless small-incision cataract surgery (SICS),[97][98] a technique which has been used to treat 4 million of the world's 20 million people with cataract blindness.
Medical colleges
Institute of Medicine, the central college of Tribhuvan University is the first medical college of Nepal and is in Maharajgunj, Kathmandu. It was established in 1972 and started to impart medical education from 1978. Other major institutions include Patan Academy of Health Sciences, Kathmandu Medical College, Nepal Medical College, KIST Medical College, Nepal Army Institute of Health Sciences, National Academy of Medical Sciences (NAMS) and Kathmandu University School of Medical Sciences (KUSMS), are also in or around Kathmandu.[99]
Economy
Central Bank of Nepal
The location and terrain of Kathmandu have played a significant role in the development of a stable economy which spans millennia. The city is in an ancient lake basin, with fertile soil and flat terrain. This geography helped form a society based on agriculture. This, combined with its location between India and China, helped establish Kathmandu as an important trading centre over the centuries. Kathmandu's trade is an ancient profession that flourished along an offshoot of the Silk Road which linked India and Tibet. From centuries past, Lhasa Newar merchants of Kathmandu have conducted trade across the Himalaya and contributed to spreading art styles and Buddhism across Central Asia.[100] Other traditional occupations are farming, metal casting, woodcarving, painting, weaving, and pottery.[101]
Kathmandu is the most important industrial and commercial centre in Nepal. The Nepal Stock Exchange, the head office of the national bank, the chamber of commerce, as well as head offices of national and international banks, telecommunication companies, the electricity authority, and various other national and international organizations are in Kathmandu. The major economic hubs are the New Road, Durbar Marg, Ason and Putalisadak.[101]
The economic output of the metropolitan area of around Rs. 550 billion approximately per year alone is worth more than one third of national GDP (nominal), while the per capita income of $2200 is approximately three times the national average.[102] Kathmandu exports handicrafts, artworks, garments, carpets, pashmina, paper; trade accounts for 21% of its revenues.[101][102] Manufacturing is also important and accounts for 19% of the revenue that Kathmandu generates. Garments and woolen carpets are the most notable manufactured products.[102] Other economic sectors in Kathmandu include agriculture (9%), education (6%), transport (6%), and hotels and restaurants (5%).[102] Kathmandu is famous for lokta paper and pashmina shawls.
Tourism
Hotel Shanker is one of the city's popular heritage hotels
Tourism is considered another important industry in Nepal. This industry started around 1950, as the country's political makeup changed and ended the country's isolation from the rest of the world. In 1956, air transportation was established and the Tribhuvan Highway, between Kathmandu and Raxaul (at India's border), was started. Separate organizations were created in Kathmandu to promote this activity; some of these include the Tourism Development Board, the Department of Tourism and the Civil Aviation Department. Furthermore, Nepal became a member of several international tourist associations. Establishing diplomatic relations with other nations further accentuated this activity. The hotel industry, travel agencies, training of tourist guides, and targeted publicity campaigns are the chief reasons for the remarkable growth of this industry in Nepal, and in Kathmandu in particular.[103] Since then, tourism in Nepal has thrived. It is the country's most important industry.[104] Tourism is a major source of income for most of the people in the city, with several hundred thousand visitors annually. Hindu and Buddhist pilgrims from all over the world visit Kathmandu's religious sites such as Pashupatinath, Swayambhunath, Boudhanath, Changunarayan and Budhanilkantha. From a mere 6,179 tourists in 1961/62, the number increased to 491,504 in 1999/2000. In economic terms, the foreign exchange registered 3.8% of the GDP in 1995/96 but then started declining. Following the end of the Maoist insurgency, there was a significant rise in the number of tourist arrivals, with 509,956 tourists recorded in 2009. Since then, tourism has improved as the country transitioned into a republic. The high level of tourism is attributed to the natural grandeur of the Himalayas and the rich cultural heritage of the country.[103]
Hyatt Regency, Kathmandu
The neighbourhood of Thamel is Kathmandu's primary "traveller's ghetto", packed with guest houses, restaurants, shops, and bookstores, catering to tourists. Another neighbourhood of growing popularity is Jhamel, a name for Jhamsikhel that was coined to rhyme with Thamel.[105] Jhochhen Tol, also known as Freak Street, is Kathmandu's original traveller's haunt, made popular by the hippies of the 1960s and 1970s; it remains a popular alternative to Thamel. Ason is a bazaar and ceremonial square on the old trade route to Tibet, and provides a fine example of a traditional neighbourhood.
With the opening of the tourist industry after the change in the political scenario of Nepal in 1950, the hotel industry drastically improved.[106] Now Kathmandu boasts several luxuries such as the Hyatt Regency, Dwarika's, Hotel Yak & Yeti, The Everest Hotel, Hotel Radisson, Hotel De L'Annapurna, The Malla Hotel, Shangri-La Hotel (not operated by the Shangri-La Hotel Group) and Hotel Shanker. There are several four-star hotels such as Akama Hotel, Hotel Vaishali, Hotel Narayani, The Blue Star and Grand Hotel. The Garden Hotel, Hotel Ambassador, and Aloha Inn are among the three-star hotels in Kathmandu. Hotels like Hyatt Regency, De L'Annapurna, and Yak & Yeti are among the five-star hotels with casinos as well.[107]
Transport
Arch bridges over the Dhobi Khola river in Baneshwor, Kathmandu
Road
The total length of roads in Nepal is recorded to be 17,182 km (10,676 mi), as of 2003–04. This fairly large network has helped the economic development of the country, particularly in the fields of agriculture, horticulture, vegetable farming, industry and also tourism.[108] In view of the hilly terrain, transportation takes place in Kathmandu are mainly by road and air. Kathmandu is connected by the Tribhuvan Highway to the south connecting India, Prithvi Highway to the west and Araniko Highway to the north connecting China. The BP Highway connects Kathmandu to the eastern part of Nepal through Sindhuli.[109] The fast-track is under construction which will be the shortest route to connect Terai with the valley.[110]
Sajha Yatayat provides regular bus services throughout Kathmandu and the surrounding valley. Other bus companies including micro-bus companies operate several unscheduled routes. Trolleybusses used to operate on the route between Tripureshwor and Suryabinayak on a 13-kilometer route.
Air
The main international airport serving Kathmandu valley is the Tribhuvan International Airport, about 6 kilometres (3.7 mi) from the city centre and is operated by the Civil Aviation Authority of Nepal.[111] It has two terminals, one domestic and one international. At present, it connects 30 cities around the globe in Europe, Asia and the Middle East such as Istanbul, Delhi, Mumbai, Bangalore, Kolkata, Singapore, Bangkok, Kuala Lumpur, Dhaka, Paro, Lhasa, Chengdu, Guangzhou and Hong Kong.[111] Since 2013, Turkish Airlines connects Istanbul to Kathmandu.[112] Oman Air also connects Muscat to Kathmandu since 2010.[113] Nepal Airlines started flying to Tokyo-Narita from March 2, 2020.[114] Regionally, several Nepali airlines operate from the city, inc
Située dans la Glorieta de D. Juan de Austria, la Fontaine des Quatre Saisons , est composée d'un bassin et de trois corps à des hauteurs différentes.
Ce bassin recueille l'eau qui tombe des corps supérieurs, qui ont la forme d'une coquille Saint-Jacques .
Dans la section entre le premier et le deuxième corps, il y a quatre reliefs qui représentent les quatre saisons de l'année.
La fontaine a été construite en 1929 par Manuel Delgado Brackenbury, avec l'aide d'Eduardo Castillo et de Manuel García.
The iconic "Beauty of Flight" sculpture that greets visitors at the main gate of the Pima Air and Space Museum in Tucson, Arizona.
The intermediate Cable Car station on the eastern ridges provides the access to the eastern cliffs with its 3 vertical chimneys and the beautiful 360-degree views. Visitors would be able to observe at close range the unique rock formations geological features of the Mat Chincang range, which was formed 500 million years ago during the Cambrian period, in geological terms.
The journey from the Base Station to Middle Station will cover 1,700 meters in length and upon reaching the Middle Station at an elevation of 650m above sea level, visitors will be able to alight and walk up to the viewing platforms.
Visitors will enjoy panoramic view of the main island as well as the many surrounding islands. They will also be able to observe at close range the unique flora on the ridges and the forested valley between the Middle Station and the Top Station. After enjoying the beautiful view, visitors will then board back the gondolas, which will take them another 450 meters up to the Top Station.
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HDR/DRI lesson is available upon request. PM me for details :)
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Terraced iron-sulphate-stromatolites formed by acid leachates from pyrite-bearing mine wastes, Tintillo river (Iberian Pyrite Belt, Riotinto Mining Basin, Huelva, Spain)
Terraced iron formations of millimetric to metric scale are usually developed during the oxidation and hydrolysis/precipitation of dissolved iron in the acidic solutions after they emerge from waste piles, tailings, or mine portals, and they display a morphological pattern similar to that observed in travertines formed in Ca2+-HCO3 ––rich spring waters. TIFs differ from calcareous travertines, however, in their mineralogical composition, which is characterized by hydrous iron (oxy)hydroxides and/or hydroxysulfates, in agreement with the typical Fe(II)/Fe(III)-SO4 2– chemical composition of most acid mine drainage solutions. These spectacular formations are the result of the interaction between (1) highly acidic and Fe(II)-enriched waters, (2) atmospheric oxygen, and (3) acidophilic microbes that have found perfect habitats for their Fe-oxidizing metabolisms in these extreme environments. The abiotic processes could be more important than the biotic factors in winter (higher flow, lower temperature), and conversely, the bacterial activity could play a major role in summer (lower flow, higher temperature).
The water from the Tintillo river (and other rivers and creeks from Riotinto Mining Basin, Huelva, Spain) has a nearly unique red and orange colour derived from its extremely acidic chemical makeup, with very high levels of iron and heavy metals. There are a number of subsurface sulfide (mainly pyrite) bodies responsible for this acidity. These mineral bodies belong to the Iberian Pyrite Belt, formed 350 My ago in the Devonian Period, connected to active and hydrothermal volcanism that led to the formation of a volcanic-sedimentary complex. Volcanic activity in the region led to eight giant volcanogenic massive sulfide ore deposits associated with polymetallic massive flanks of volcanic cones in the form of pyrite, but also chalcopyrite, sphalerite, galena and cassiterite.
References:
Iron terraces in acid mine drainage systems: A discussion about the organic and inorganic factors involved in their formation through observations from the Tintillo acidic river (Riotinto mine, Huelva, Spain)
pubs.geoscienceworld.org/gsa/geosphere/article-pdf/3/3/13...
The Tintillo acidic river (Rio Tinto mines, Huelva, Spain): an example of extreme environmental impact of pyritic mine wastes on the environment or an exceptional site to study acid-sulphate mine drainage systems?
www.researchgate.net/publication/235355068_The_Tintillo_a...
Common Lizard (Zootoca vivipara), melanistic form. Higher Bosistow Cliff, St Levan, Cornwall. Sunday 16th April 2017.
My Wild Guide describes the occurrence of this colour form as 'frequent', though this was the first time that I've encountered one.
Hier kann man anhand der Form des Teiches, der die Form eines Hufeisens hat, nachvollziehen, wie die Hufeisensiedlung zu ihrem Namen kam. Das Ensemble rund um diesen Teich hat in etwa die gleiche Form.
Die Hufeisensiedlung im Berliner Ortsteil Britz ist eine Siedlung des sozialen Wohnungsbaus und seit 2008 UNESCO-Welterbe. Sie entstand nach Plänen des Architekten Bruno Taut, des Architekten und späteren Berliner Stadtbaurats Martin Wagner sowie des Gartenarchitekten Leberecht Migge. Sie ist eines der ersten Projekte des sozialen Wohnungsbaues und gilt als eine Ikone des modernen Städtebaus und des Neuen Bauens.
Die Siedlung wurde zwischen 1925 und 1933 in mehreren Bauabschnitten errichtet, von denen die zwischen 1925 und 1930 errichteten ersten sechs Abschnitte seit 1986 gemeinsam als Ensemble unter Denkmalschutz stehen. 2008 wurde die Hufeisensiedlung gemeinsam mit fünf anderen Berliner Wohnsiedlungen zum UNESCO-Welterbe Siedlungen der Berliner Moderne ernannt. Die seit 2010 zudem als Gartendenkmal eingetragene, nach dem zentralen Bauteil in Form eines Hufeisens benannte Siedlung ist außerdem Teil der ab 1925 in direkter Konkurrenz von zwei unterschiedlichen Wohnungsbaugesellschaften (GEHAG und Degewo) errichteten Großsiedlung Britz. Der dem Hufeisen gegenüberliegende Bauteil der DeGeWo, die so genannte „Krugpfuhlsiedlung“, wurde ebenfalls ab 1925 errichtet und von den Architekten Ernst Engelmann und Emil Fangmeyer in deutlich traditionellerer Formensprache entworfen
de.wikipedia.org/wiki/Hufeisensiedlung
www.stadtentwicklung.berlin.de/denkmal/liste_karte_datenb...
de.wikipedia.org/wiki/Berlin-Britz
de.wikipedia.org/wiki/Siedlungen_der_Berliner_Moderne
de.wikipedia.org/wiki/Bruno_Taut
de.wikipedia.org/wiki/Martin_Wagner_(Architekt)
Pink form of an Angulose Prominent (Peridea angulosa) on Oak (Quercus sp.). Catoctin Mountains, Frederick County, Maryland.
uno scatto di qualche settimana fa al porto di Formia...
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Odda is a town and administrative center in Ullensvang municipality in Vestland county in Norway. The town is located deep in the Sørfjorden in Hardanger , and has 4,764 inhabitants as of 1 January 2023 . Odda was the administrative center of Odda municipality , which on 1 January 2020 was merged with Jondal and Ullensvang to form the new Ullensvang municipality.
In 2009 , the industrial heritage in Odda-Tyssedal was listed on Norway's tentative list for UNESCO's World Heritage List , together with the Rjukan–Notodden industrial heritage .
Public services
Odda hospital is a local hospital for the municipalities of Eidfjord, Jondal, Odda and Ullensvang.
Odda secondary school offers both vocational and study specialist educations.
Business
Odda is known as an industrial location, with companies such as Odda Smelteverk , Boliden Odda (formerly Norzink ) and Tinfos Titan & Iron (TTI).
History
Tourism and hotel management
Before industrial activity in Odda began around 1910, Odda was a popular tourist destination which, among other things, attracted many foreigners who wanted to experience the scenic area with glaciers, fjords and waterfalls. This laid the foundation for several people to start hotel operations on the site.
Some of the most popular destinations for tourists visiting Odda were Låtefossen and Espelandsfossen .
Shuttle station, steamship wharf and steamship expedition
Baard Jakobsen Aga (1812–1895) received a merchant license in Odda in 1861, and in 1864 took over the shuttle station that was in operation in Odda. Then he secured a new plot of land where he built a hotel which was called alternately Prestegårds Hotel and Agas Hotel. In 1868 he became a post opener and steamship dispatcher, and he then had a steamship wharf and dispatch house built at Almerket. He had previously expanded the hotel business, but in 1888 he inaugurated a new hotel building, the "new Agas Hotel". In the 20th century, the large hotel building was used for other purposes, including Rita's bakery, which led to the building being called "Ritagården" colloquially. Agas Hotel/Ritagården was demolished in 1978.
From guest house to Hotel Hardanger
The start of hotel operations at Odda occurred around 1845, when a man named Monsen started an inn on the site. Monsen went bankrupt in the 1860s, and the inn was bought by a man named Wetshus. He continued to run the hotel business. After Wetshus had died, the two brothers Sven and Mikal Tollefsen became his successors in the early 1880s, with financial support from a rich Englishman. The Tollefsen brothers carried out a major renovation of the former guest house. When Sven Tollefsen died, Mikal Tollefsen became the hotel's sole owner.
Tollefsen also bought Agas Hotel, which Baard Jakobsen Aga had started.
On 9 August 1895, the then Hotel Hardanger was completely damaged in a fire. The fire started in Hotel Hardanger, but 7–8 neighboring buildings also caught fire. It was said that the fire was caused by the maid of an English hotel guest having left a candle or a kerosene lamp by an open window, and that the curtain had caught fire - as it was very hot most of the windows in the hotel were open, and this caused the fire to spread with great speed. The fire started at 12 o'clock in the morning.
The commander and crew of the steamship "Vega" - which happened to be docked in Odda when the fire started - managed to put out the fire(s) within three hours using fire-fighting equipment from the ship. Among other things, they managed to save the post office, while the telegraph building was lost. The competing Jordals Hotel, which was run by Jacob Jordal, was also saved.
Hotel Hardanger was insured, and Bergens Tidende wrote that the insurance sum was NOK 90,000, but also published an anonymous source's assessment that the hotel complex was worth NOK 200,000–250,000, and that the owner - Mikal Tollefsen - had probably suffered a significant financial loss due to underinsurance. No people were injured in the fire.
Shortly after the fire in 1895, Tollefsen started building a new and larger hotel on the site of the fire. The new hotel was completed on 24 June 1896, and had 170 hotel beds in 110 guest rooms. Architecturally, it was a mixture of Swiss style and dragon style, with towers and projections.
Hardanger Hotel is mentioned, among other things, in a French travelogue published in 1897.
In 1913, the owner of Hotel Hardanger filed a claim for damages against the two factories - a cyanamide factory and a carbide factory - which had started up in Odda a few years earlier, because the factory operation caused such great pollution and bad odors that it affected the hotel operation. The provisions of the Neighborhood Act were the legal basis for the lawsuit. The court agreed with the plaintiff that the two factories were obliged to pay compensation for inconvenience and losses that the hotel had suffered after 2 August 1911, but not because Odda had become less idyllic and thus attractive to tourists. The compensation sum was to be determined after an appraisal had been carried out , and the result of the appraisal was not available until 1922. By then both factories had gone bankrupt, and hotel owner Mikal Tollefsen had died.
Hotel Hardanger becomes a town hall
In 1917, the municipality bought the Hotel Hardanger, to convert the building into a town hall . The hotel had then been almost empty all year round, because the industrial activity on the site had meant that the tourists did not show up. [9]
The hotel's so-called "Kongerom" was converted into a chairman's office and lord's boardroom. Eventually, the new town hall also accommodated a number of other businesses, such as a cinema, police station, doctor's office and bank. The old hotel was in use as Odda Town Hall until a new building was inaugurated in 1957; from then on, the former Hotel Hardanger was referred to as Odda old town hall . This building was demolished in 1976.
Jordals Hotel becomes Hardanger Hotel
In 1917, Jordals Hotel was bought by the Melkeraaen family, who continued to run the hotel for 68 years. Along the way, they changed the name of the hotel to Hardanger Hotel.
The Hardanger Hotel, which was a wooden Swiss-style building, was demolished in 1962, and a new five-story hotel building was inaugurated on 1 July 1963.
From tourism to industrial site
Factories and smelters
At the beginning of the 20th century, two factories were started in Odda. On one, cyanamide was produced, and on the other, carbide was produced .
In 1908, the operation of the first factory that was to be part of Odda Smelteverk , a carbide factory owned by a British company, began. In 1909, another British company started production of calcium cyanamide in the same area as the first factory. The reason why Odda was interesting for the foreign companies was the access to large amounts of hydropower and ice-free ports.
Both factories went bankrupt in 1921 , in connection with the worldwide economic crisis that occurred in the early 1920s. The bankruptcies led to thousands of people becoming unemployed. Both factories started up again in 1924, with Odda Smelteverk A/S as the new owner. This operating company was established by the power company Tyssefaldene and the Hafslund/Meraker group.
The cyanamide factory was built on in the 1930s.
At the smelter, the so-called Odda process was developed by chief chemist Erling Johnson in 1927–1928; it is a chemical process based on nitric acid for the industrial production of three-sided artificial fertilizer with the sub-components nitrogen , phosphorus and potassium .
Preservation decision and dispute over conservation value
In 2011 , the National Archives decided to protect several of the smelter's buildings and facilities, and to include the smelter in the Norwegian application to UNESCO for world heritage status for Norwegian industrial monuments. In 2013, however, the Ministry of the Environment decided that the series nomination should be split into two phases, 1. application for Rjukan/Notodden to be submitted to UNESCO in January 2014, and phase 2, that work be continued on expanding the nomination to include Odda/ Tyssedal with eventual submission to UNESCO in January 2016.
The owners of the smelter site objected to the conservation decision made in 2011, but the decision was upheld in 2012. The conservation included the cyanamide factory, the cable car, the Linde house (named after the German inventor Carl von Linde ) and the limestone silo on the import quay. Over the years, there has been much controversy in Odda about whether the smelter's buildings and facilities should be preserved or removed.
Cultural life
Music and theater
Tyssedalkoret and Odda Songlag are two choirs that come from Odda municipality. The water power and industrial history of the area here was documented in the performance and the DVD ``Arven'', performed by Tyssedalkoret with band and soloists in autumn 2004 and released on DVD in Christmas 2005. In addition these two choirs have the bands Odda Musikklag , Odda Skolekorps and Røldal Skolemusiklag. The blues team Lokst Utøve has 272 members. The Blueslaget received the culture award for 2009 for their great work as concert/festival organisers, volunteer workers and inspirers for bands and soloists. In 2011, Erlend Garatun Huus published the book Rock og Røyk , which is about the history of rock in Odda.
At the closed smelter (2001), the old "Lindehuset" has been used for theater and concert activities. The theater play Bikebubesong , based on the Oddingen Frode Grytten's novel Bikubesong , was performed in this venue in 2003 with great success. The play's performance in Oslo has been the most watched contemporary drama in Norwegian history.
A key cultural player in Odda is the company Oddakonsertene, led by Gunn Gravdal Elton. In April 2019, the Odda concerts staged the musical Albert og Leonie , a story about how Odda arose as an industrial community. The musical was a huge success with sold-out houses. 2,600 people queued to see and hear the story. The director was Martine Bakken Lundberg. The main roles were played by André Søfteland and Lene Kokai Flage. Over 60 amateurs were on stage. Albert and Leonie was planned to be staged again in 2020 and 2021, but had to be canceled due to the corona pandemic .
The odd concerts started in 2005 and as of 2019 have staged more than 60 concerts. All have been sold out. The most popular concerts are the annual Christmas concerts, which gather over 1,000 listeners. The traditional Christmas concert in Odda church with a large ensemble and two to three concerts in a row officially ended in 2019, but a simplified version was arranged in 2020, with concerts in Skare and Odda churches.
The Literature Symposium
From 2005, a festival called the Literature Symposium in Odda has been organized every autumn . The Linden house at the defunct Smelteverket, Odda cinema, Sentralbadet, Odda church are some of the venues at the symposium. Previously, there was every year "Bikubegang" with Frode Grytten , where he told about the story behind the book "Bikubesong", while he wandered around Odda. The literary symposium also has concerts, often in connection with an author/musician or individual artists. During the Literary Symposium 2011, the Sentralbadet Litteraturhus opened in the old bathroom at the closed Smelteverket, and this has become headquarters for the symposium, as well as a permanent house for literary events all year round.
As of 2010, a major rehabilitation/remodeling of Lindehuset was planned, so that the building would be better suited for events such as concerts and theater performances.
The National Antiquities' "Value creation project"
Odda is one of the pilot projects in the Value Creation Project for the National Archives.
TV shows
The actions in the TV series RIP Henry and Ragnarok have been added to Odda, and are recorded there. In Ragnarok, on the other hand, the city goes by the name Edda .
Known oddities
Samson Isberg (1795–1873), sharpshooter
Knud Knudsen (photographer) (1832–1915)
Gro Holm , born Prestgarden (1878–1949), writer
Alfred Hagn (1882–1958), painter, writer and spy.
Claes Gill (1910–1973), writer, actor and theater manager
Torbjørn Mork (1928–1992), doctor, politician ( Ap ), director of health 1972–1992
Walther Aas (1928–1990), artist
Roger Albertsen , (1957–2003), footballer
Anne B. Ragde (born 1957), writer, (raised in Trondheim)
Arne Borgstrøm (born 1959), elite long-distance swimmer
Frode Grytten (born 1960), author
Lars Ove Seljestad (born 1961), author
Bjørn Ingvaldsen (born 1962), author, leader of Norwegian Children's and Young People's Book Writers
Hallgeir Opedal (born 1965), writer and journalist
Børge Brende (born 1965), politician ( H ), former secretary general of the Norwegian Red Cross , minister of foreign affairs
Ida Melbo Øystese (born 1968), chief of police in Oslo from 2023.
Knut Olav Åmås (born 1968), author, editor, director of the foundation Fritt Ord
Leif Einar Lothe (born 1969), entrepreneur, singer, TV profile
Marit Eikemo (born 1971), writer
Tore Aurstad (born 1972), author
Ingvill Måkestad Bovim (born 1981), athlete
Håkon Opdal (born 1982), footballer
Ingvild Skare Thygesen (born 1993), TV profile
The Sognefjord is Norway's longest and deepest fjord with its 205 km and 1303 m at its deepest (SNL states 1308), including Sognesjøen which is at the far end towards the North Sea. The Sognefjord has the deepest point on Norway's coast. The fjord is 176–180 km from the innermost Lusterfjorden ( Skjolden ) to Sognefest , and 206 km to the outermost reef (then Lake Sognesjøen is also included). The width varies from around 1 to 2 km in Lusterfjorden to 4–5 km from Leikanger and beyond. Measured from the threshold to Skjolden, the fjord is 174 km. The middle part of the fjord is surrounded by mountains of around 1000 meters and in the inner part the height difference between the bottom of the fjord and the mountain tops is 3500 metres. The highest peak right by the fjord is Bleia at 1,721 metres, which gives a 2,850 meter height difference. Around the inner part of the fjord, the landscape is alpine with pointed mountain peaks, steep mountain sides and glaciers. As an extension of the fjord arms, long and deep valleys extend in all directions, including Jostedalen , Lærdalen and Årdal with Utladalen . The Sognefjord is the world's longest open (ice-free) fjord. The Sognefjord is the world's third longest fjord.
It is located in the middle of Vestland county (formerly Sogn og Fjordane county to which it helped give its name) and stretches from Solund on the coast in the west to Skjolden at the foot of Jotunheimen in the east (northeast), where the fjord arm is called Lustrafjorden . The fjord and the land around it make up the Sogn region, often divided into Outer, Midtre and Indre Sogn. The length from Rutletangen to Skjolden is 186 km . Sogn makes up almost 60% of the area in Sogn and Fjordane, or around 11,000 km 2 . The twelve municipalities in Sogn have a total area of 10,671.55 km² and 37,063 inhabitants (1 January 2014). The land around the inner part of the fjord is called Indre Sogn and includes the long fjord arms. From Leikanger onwards, the country is called Ytre Sogn . The outer part of the fjord has few and small fjord arms. The fjord arms are like hanging valleys under water in that the bottom in the side fjords is often much shallower than the main fjord with a height difference of over 1,000 meters in some cases. The main fjord has a threshold at its mouth to the sea, while several of the side fjords have thresholds at the mouth of the main fjord.
The Sognefjord cuts so deeply into the country that it is only 15 km from the innermost arm at Skjolden to mountain peaks such as Store Skagastølstind in Jotunheimen. The water flow usually exits the fjord. The rivers create sandbanks where they run into the fjord, for example at Gudvangen, in Lærdal and in Gaupne. These sandbars are constantly expanding and changing shape.
The Sognefjord, especially the inner part, is surrounded by mountain massifs which are alpine in the inner part and more rounded in the outer part. The innermost arms of the fjord continue as deep and sometimes long valleys, including Lærdal , Årdal with Utladalen , Nærøydalen , Sogndalsdalen , Fjærland , Fortunsdalen , Aurlandsdalen and Jostedalen . The transition between the fjord and these valleys is determined by sea level, and the boundary has moved outwards at the uplift. Some of the side valleys, such as Vik and Fresvik, would have been hanging valleys in the same way as the Feigedalen if the Sognefjord was drained.
Name
Amund Helland writes " The Sognefjord's real name is Sogn , while Sogn is now used only for the surrounding landscape, and was thus already used in the Middle Ages. As a landscape name, the name is a masculine word and has undoubtedly been so as a fjord name as well." The name is connected to the word "suction", which probably refers to the suction or the difficult current conditions that are created when the water flows through the fjord mouth and over the threshold.
Geography
Large parts of the fjord are surrounded by steep mountains. Kvamsøy at Balestrand is a small island separated from the mainland by a short, shallow strait. Outside Balestrand there are small fjord arms and at Veganes ( Dragsvik ferry quay ) there is a significant branching with the Fjærlandsfjorden .
Municipalities
Municipalities with shoreline to the fjord, counted from west to east:
Solund
Hyllestad (north side)
Gulen (south side)
Høyanger (on both sides of the main fjord)
Vik (south side)
Sogndal (north side)
Aurland (south side, around the Aurlandsfjord)
Lærdal (south side)
Luster (north side, around Lustrafjorden)
Årdal (around the Årdalsfjord)
Depths
The Sognefjord has only one threshold which is at the mouth and the threshold is around 165 meters deep. The area beyond the threshold is called Sognesjøen , which is sheltered by islands to the north and south; there is no threshold outside Sognesjøen that has free circulation towards the ocean.
From the inner parts at Årdal or Skjolden, the fjord gradually deepens outwards (westwards). Between Fodnes-Mannheller and Rutledal-Rysjedalsvika, the bottom is at least 800 metres. The deepest part is approximately at Åkrestrand and Vadheim. The outer part of the fjord (at Losna and Sula ) has a marked threshold with depths of 100 to 200 metres, where the fjord bed rises abruptly from a depth of 1,200 meters to around 100 meters over a stretch of 5 km at Rutledal. In Lake Sognesjøen there are several small troughs (with depths down to 400-500 metres) with thresholds between them. Across the fjord, the bottom is partly completely flat with less than 1 meter variation in depth over a 2 km cross-section. The bottom is covered by fine material (clay) which at Vangsnes is up to 300 meters thick. Seismic shows that the greatest depth to the bedrock is approximately 1,600 m, but loose masses with a thickness of 200–400 m mean that the fjord bottom is nevertheless flat. Seismic surveys at Vangsnes have revealed a 300 meter thick layer of clay at the bottom.
Between 50 and 180 km from the mouth, the fjord bed is relatively flat. Almost all side fjords form hanging valleys to the main fjord. For example, the mouth of the Fjærlandsfjord is well over 400 meters deep, while the main fjord is close to 1,200 meters deep just outside the mouth. Vadheimfjord's mouth is 400 meters deep, here the greatest depth is over 1300 m. Ikjefjord's mouth is only 50 meters deep close to where the main fjord is at its deepest. In large parts of the fjord, it is "abruptly deep" in that the steep mountain sides continue just as steeply underwater.
In contrast to a number of other fjords, not every single part of the Sognefjord has its own name. Only the outermost part has its own name - Sognesjøen . However, there are many fjord arms. From west to east these are:
Sognesjøen
Straumsfjorden
Bjørnefjorden
Nessefjord
The Sognefjord
Lifjorden
Bøfjorden
The Risnefjord
The Ikjefjord
Vadheimsfjorden
Fuglsetfjorden
Høyangsfjorden
Lånefjorden
The Finnafjord
The Arnafjord
The Inner Fjord
Framfjorden
Vikbukti
The Esefjord
Fjærlandsfjorden
The Vetlefjord
Sværefjorden
The Norafjord
Sogndalsfjorden
Barsnes Fjord
The Eidsfjord
Aurlandsfjorden
The Nærøyfjord
Amla Bay
Lærdalsfjorden
Årdalsfjorden
The Lustrafjord
The Gaupnefjord
Climate and fresh water
The fjord colored by meltwater from the glacier.
Terrain formations and distance to the sea lead to great variations in climate along the fjord. The outer part has a mild and humid coastal climate, while the innermost part has an inland climate with cold and dry winters.
The amount of precipitation decreases strongly inwards into the fjord. Lærdal lies in the rain shadow and has very little rainfall, while west-facing slopes further out have a lot of rainfall and there the rainfall often increases with altitude. Brekke and Takle in Ytre Parish are among the places in Norway with the most rainfall. North of the Sognefjord lies the Jostedalsbreen, Norway's largest glacier, and parts of the meltwater drain into the Sognefjord. Wind conditions are strongly influenced by terrain formations. In winter, the dominant wind direction is out the fjord or out the side valleys in the form of so-called downwinds . Fall winds can be very strong and have a major impact on cooling and icing. The slopes and valleys along the inner parts of the fjord have a partially mild climate and are fertile, which makes the area suitable for growing fruit and berries, among other things. The slopes along the fjord partly have large conifer forests, including in the roadless area of Frønningen .
The fjord receives fresh water mainly from the rivers and very little precipitation directly on the fjord's water surface. In the inner part of the Sognefjord, the total supply of fresh water during one year corresponds to a depth of 33 meters if it were distributed over the entire area of the fjord. In spring and partly in autumn, the top 2-3 meters of the fjord are brackish water , especially in the side fjords. The salt content in the surface is lowest in summer and autumn. In June 1954, for example, 5 ‰ salt was measured in the uppermost meters of the Lustrafjord, while at great depths it was 34.5 ‰. Regulation of the waterways for power production has led to a larger proportion of fresh water flowing into the fjord in the winter. The most extensive regulation is in Aurland, Lærdal, Årdal and Jostedal. Regulations affect temperature in the surface layer and icing. In the inner part of the fjord, the rivers are fed by high mountains and glaciers.
The rivers Lærdalselvi , Aurlandselvi , Flåmselvi , Mørkridselvi , Henjaelvi , Grindselvi , Hamreelvi , Njøsaelvi , Kvinnafossen , Sogndalselvi and Jostedøla flow into the Sognefjord and normally have spring floods in June. [3] Lærdalselva has the largest catchment, followed by Jostedøla and Aurlandselva, and these three have roughly the same water flow (around 40 m 3 /second). The Årdalsvatnet drains to the Sognefjord through the short Åreidselva or Hæreidselvi through the Årdalstangen . The Eidsvatnet in Luster drains into the Sognefjord just by Mørkridselvi in Skjolden . Regulation of the waterways for hydropower has resulted in a more steady supply of fresh water throughout the year. Without regulation, 92% of the fresh water would have been supplied in the summer half-year from May to October. Several of the large rivers flow into fjord arms.
Geology
The bedrock along the outer and middle part of the fjord consists mostly of Precambrian gneiss with orientation east-west and northeast-southwest. The islands of Solund consist mostly of Devonian sandstone and conglomerates , while the interior (eastern part) consists mostly of Caledonian gabbro , anorthosite , granite and phyllite .
Jostedøla's material transport (in the form of sludge) involves sedimentation in the Gaupnefjord of 10 to 20 cm/year near the river basin, and 1 cm/year 2 km from the river basin. The river transports 50,000 to 100,000 tonnes of silt annually. The sludge concentration from Jostedøla is at most 1 g/litre. It is particularly at Gaupne that the meltwater from the glaciers is marked by the color of the water.
Icing
According to Helland, it was common for the ice to settle on several of the fjord arms every winter, including on Aurlandsfjorden, Nærøyfjorden and Årdalsfjorden. In the winter of 1888–1889, Lusterfjorden was iced over for six months straight. In the deepest parts of the Sognefjord, there is a year-round temperature of around 6.5 °C, according to Helland. Outer parts are almost never iced over, not even the side fjords. The inner parts can be frozen for several weeks at a stretch. Among other things, inner parts of the Aurlandsfjorden and the Nærøyfjorden freeze easily. Lærdalsfjorden is usually ice-free except for the very innermost part, while it has happened that Årdalsfjorden has been iced up to Ofredal and has been an obstacle to ship traffic. Historically, Lustrafjorden has often been iced over as far as Urnes. The Barsnesfjorden has often been covered with ice. In the Nærøyfjord it happened (among other things in the 1920s and in 1962) that the liner was unable to enter the fjord due to ice and had to dispatch at the ice edge.
Streams
In the Sognefjord, incoming current is hardly noticeable and is most noticeable in strong westerly winds. Outgoing current dominates and is particularly strong in spring and summer. At strong tides, the tidal flow can reach over 1 m/s (2 knots ) around the pier and headland. The Sognefjord is covered by a layer or stream of brackish water of up to 10 meters (varying with the seasons and supply from the rivers). Beneath the brackish water, a current or intermediate layer at a depth of 150 meters goes in and out of the fjord and below this lies the main basin, which has some connection with the ocean beyond the threshold. Together, these three currents contribute to the fact that the water in the fjord is replaced on average within 8-10 years, so that the fjord has life right down to the bottom. The brackish water layer has less density and therefore does not mix easily with the deeper layers. The brackish water that flows out of the fjord slowly mixes with the layer below so that the salt content increases at the same time as the brackish water layer increases up to 10 times the amount of fresh water supplied. The brackish water that flows towards the mouth must be replaced and sets up an incoming current in a slightly deeper layer.
Fish
The Sognefjord has herring and good sprat fishing . In the outer parts of the fjord, salmon has traditionally been fished with wedge nets . Salmon warp or "sitjenet" is a traditional method of salmon fishing and skilled players could catch a lot of fish with this method. Hook nets and drift nets have dominated in modern times and do not require the same active fishing as warp . The salmon's migration in the fjord is controlled by currents on the surface and the warps are placed where there are favorable current conditions where, due to the current, the salmon are driven close to land on their way into the fjord. In Leikanger and Balestrand there are many good places for sitejnot with Suppham being by far the best. Good salmon rivers such as Lærdalselva, Aurlandselva and Årøyelva flow into the Sognefjorden.
In the outer part of the fjord (Gulen and Solund) there is some fish farming. Several of the waterways are known for good salmon and sea trout fishing , and five of the rivers have been designated as national salmon rivers. Lærdalselva has a salmon-carrying stretch and has had by far the largest population. Aurlandselva has historically had a good catch of sea trout. The Sognefjord is among the most important in Norway for anadromous fish species. Norwegian spring-spawning herring are fished in the fjord, especially in the outer parts, as well as some coastal sprat.
In the Sognefjord there are plankton algae which in other Norwegian waters and the occurrence follows the seasons. In general, there is little occurrence in winter due to low light, diatoms bloom in March-April and are dependent on the supply of nutrient salts, in May-June diatoms and flagellates bloom in connection with the spring flood, in summer there is a varying population, new blooms in the autumn in connection with, among other things, floods, and married species can occur all year round.
Tourism
The Sognefjord was established as a tourist destination in the 19th century, among other things, with the establishment of Fylkesbåtane. One of the targets was Gudvangen, which in 1889 received 79 large tourist ships with a total of over 10,000 passengers. In 1889, 4,500 travelers came with the county boats. The German Emperor Wilhelm visited the Sognefjord and Balestrand for the first time in 1890. The emperor subsequently visited the Sognefjord 25 times. The fjord itself and the surrounding area with Jotunheimen, Jostedalsbreen and several stave churches have made the Sognefjord one of Norway's most prominent tourist destinations. Balestrand, Vangsnes, Aurland and Fjærland were among the early destinations for English tourists in the 19th century.
History
It has been the Guest of Death
It has sailed on a Torden
It is christened in Rædsler vorden
that has plowed the Sognefjord
from Forthun to Sognefæst.
If you have forgotten your Lord's Prayer,
do you remember a prayer to pray:
learn it from the wrath of God!
imagine, Sinder, then present
in a Bath on Sognefjord!
Henrik Wergeland
The Sognefjord has been an important transport artery since ancient times. The gulation was probably held near the mouth of the Sognefjord and probably because it was practical to hold the meeting where the ship lay along the coast met the great fjord. From the innermost arms of the fjord it is a relatively short distance to the inland villages of Eastern Norway, particularly through Lærdal to Valdres over the moderate mountain pass Filefjell . Lærdalsøyri was from the 17th century an important market and meeting place. There, farmers from Valdres, Hallingdal and Gudbrandsdalen sold slaughter, tar and other products from the interior and bought fish, salt, hemp and iron from the fjords and from Bergen. Around 1300, the authorities established a shuttle station at Maristova at the entrance to Filefjell. The first drivable road between east and west was built over Filefjell in 1792. From 1843 the paddle steamer "Constitutionen" plyed the route between Bergen and Lærdal, the county boats took over the route in 1857. The road over the Sognefjellet was built as a carriageway in 1938. The Flåmsbana connected the Sognefjord to the railway network in 1940. Stalheimskleivi , between Voss and Sogn, was built in 1850 and turned into a road in 1937. It has made it possible to transport agricultural products , fruit , berries and fish between the villages in Sogn and Bergen .
From 1785, the Trondhjem postal route crossed the Sognefjord by boat between Rutledal and Leirvik in Hyllestad . In 1647, a postal route was established between Bergen and Christiania. The post then took 7-8 days via Gudvangen, Lærdal and Valdres.
It was difficult to get to the Sognefjord by sailboat and the yachts could lie for many days or several weeks at the mouth waiting for favorable wind conditions. East wind was favorable out of the fjord, while south to Bergen, wind from the north or north-west was needed. To enter the fjord, a wind from the west was necessary. The steam and motor boats revolutionized transport on the fjord and these had completely taken over in the early 20th century The county boats were established in 1858 with boat routes on the Sognefjord and to Bergen as an important activity.
In 1934, a ferry route was established along the fjord from Vadheim to Lærdal. From 1939 until the Lærdal tunnel opened, there was a car ferry between Gudvangen and Lærdal - first the ferry went to Lærdalsøyri itself, from 1966 to Revsnes when a road was built there to shorten the ferry route. In the 1990s, the ferry connection Revsnes-Kaupanger was replaced by Mannheller-Fodnes , and after this Kaupanger has only been used by the tourist route Gudvangen-Kaupanger-Lærdal. The road system between Sogndal and Jølster on national highway 5 , including the Fjærlands tunnel , created a ferry-free road connection on the north side of the fjord.
Norway , officially the Kingdom of Norway , is a Nordic , European country and an independent state in the west of the Scandinavian Peninsula . Geographically speaking, the country is long and narrow, and on the elongated coast towards the North Atlantic are Norway's well-known fjords . The Kingdom of Norway includes the main country (the mainland with adjacent islands within the baseline ), Jan Mayen and Svalbard . With these two Arctic areas, Norway covers a land area of 385,000 km² and has a population of approximately 5.5 million (2023). Mainland Norway borders Sweden in the east , Finland and Russia in the northeast .
Norway is a parliamentary democracy and constitutional monarchy , where Harald V has been king and head of state since 1991 , and Jonas Gahr Støre ( Ap ) has been prime minister since 2021 . Norway is a unitary state , with two administrative levels below the state: counties and municipalities . The Sami part of the population has, through the Sami Parliament and the Finnmark Act , to a certain extent self-government and influence over traditionally Sami areas. Although Norway has rejected membership of the European Union through two referendums , through the EEA Agreement Norway has close ties with the Union, and through NATO with the United States . Norway is a significant contributor to the United Nations (UN), and has participated with soldiers in several foreign operations mandated by the UN. Norway is among the states that have participated from the founding of the UN , NATO , the Council of Europe , the OSCE and the Nordic Council , and in addition to these is a member of the EEA , the World Trade Organization , the Organization for Economic Co-operation and Development and is part of the Schengen area .
Norway is rich in many natural resources such as oil , gas , minerals , timber , seafood , fresh water and hydropower . Since the beginning of the 20th century, these natural conditions have given the country the opportunity for an increase in wealth that few other countries can now enjoy, and Norwegians have the second highest average income in the world, measured in GDP per capita, as of 2022. The petroleum industry accounts for around 14% of Norway's gross domestic product as of 2018. Norway is the world's largest producer of oil and gas per capita outside the Middle East. However, the number of employees linked to this industry fell from approx. 232,000 in 2013 to 207,000 in 2015.
In Norway, these natural resources have been managed for socially beneficial purposes. The country maintains a welfare model in line with the other Nordic countries. Important service areas such as health and higher education are state-funded, and the country has an extensive welfare system for its citizens. Public expenditure in 2018 is approx. 50% of GDP, and the majority of these expenses are related to education, healthcare, social security and welfare. Since 2001 and until 2021, when the country took second place, the UN has ranked Norway as the world's best country to live in . From 2010, Norway is also ranked at the top of the EIU's democracy index . Norway ranks third on the UN's World Happiness Report for the years 2016–2018, behind Finland and Denmark , a report published in March 2019.
The majority of the population is Nordic. In the last couple of years, immigration has accounted for more than half of population growth. The five largest minority groups are Norwegian-Poles , Lithuanians , Norwegian-Swedes , Norwegian-Syrians including Syrian Kurds and Norwegian-Pakistani .
Norway's national day is 17 May, on this day in 1814 the Norwegian Constitution was dated and signed by the presidency of the National Assembly at Eidsvoll . It is stipulated in the law of 26 April 1947 that 17 May are national public holidays. The Sami national day is 6 February. "Yes, we love this country" is Norway's national anthem, the song was written in 1859 by Bjørnstjerne Bjørnson (1832–1910).
Norway's history of human settlement goes back at least 10,000 years, to the Late Paleolithic , the first period of the Stone Age . Archaeological finds of settlements along the entire Norwegian coast have so far been dated back to 10,400 before present (BP), the oldest find is today considered to be a settlement at Pauler in Brunlanes , Vestfold .
For a period these settlements were considered to be the remains of settlers from Doggerland , an area which today lies beneath the North Sea , but which was once a land bridge connecting today's British Isles with Danish Jutland . But the archaeologists who study the initial phase of the settlement in what is today Norway reckon that the first people who came here followed the coast along what is today Bohuslân. That they arrived in some form of boat is absolutely certain, and there is much evidence that they could easily move over large distances.
Since the last Ice Age, there has been continuous settlement in Norway. It cannot be ruled out that people lived in Norway during the interglacial period , but no trace of such a population or settlement has been found.
The Stone Age lasted a long time; half of the time that our country has been populated. There are no written accounts of what life was like back then. The knowledge we have has been painstakingly collected through investigations of places where people have stayed and left behind objects that we can understand have been processed by human hands. This field of knowledge is called archaeology . The archaeologists interpret their findings and the history of the surrounding landscape. In our country, the uplift after the Ice Age is fundamental. The history of the settlements at Pauler is no more than fifteen years old.
The Fosna culture settled parts of Norway sometime between 10,000–8,000 BC. (see Stone Age in Norway ). The dating of rock carvings is set to Neolithic times (in Norway between 4000 BC to 1700 BC) and show activities typical of hunters and gatherers .
Agriculture with livestock and arable farming was introduced in the Neolithic. Swad farming where the farmers move when the field does not produce the expected yield.
More permanent and persistent farm settlements developed in the Bronze Age (1700 BC to 500 BC) and the Iron Age . The earliest runes have been found on an arrowhead dated to around 200 BC. Many more inscriptions are dated to around 800, and a number of petty kingdoms developed during these centuries. In prehistoric times, there were no fixed national borders in the Nordic countries and Norway did not exist as a state. The population in Norway probably fell to year 0.
Events in this time period, the centuries before the year 1000, are glimpsed in written sources. Although the sagas were written down in the 13th century, many hundreds of years later, they provide a glimpse into what was already a distant past. The story of the fimbul winter gives us a historical picture of something that happened and which in our time, with the help of dendrochronology , can be interpreted as a natural disaster in the year 536, created by a volcanic eruption in El Salvador .
In the period between 800 and 1066 there was a significant expansion and it is referred to as the Viking Age . During this period, Norwegians, as Swedes and Danes also did, traveled abroad in longships with sails as explorers, traders, settlers and as Vikings (raiders and pirates ). By the middle of the 11th century, the Norwegian kingship had been firmly established, building its right as descendants of Harald Hårfagre and then as heirs of Olav the Holy . The Norwegian kings, and their subjects, now professed Christianity . In the time around Håkon Håkonsson , in the time after the civil war , there was a small renaissance in Norway with extensive literary activity and diplomatic activity with Europe. The black dew came to Norway in 1349 and killed around half of the population. The entire state apparatus and Norway then entered a period of decline.
Between 1396 and 1536, Norway was part of the Kalmar Union , and from 1536 until 1814 Norway had been reduced to a tributary part of Denmark , named as the Personal Union of Denmark-Norway . This staff union entered into an alliance with Napoléon Bonaparte with a war that brought bad times and famine in 1812 . In 1814, Denmark-Norway lost the Anglophone Wars , part of the Napoleonic Wars , and the Danish king was forced to cede Norway to the king of Sweden in the Treaty of Kiel on 14 January of that year. After a Norwegian attempt at independence, Norway was forced into a loose union with Sweden, but where Norway was allowed to create its own constitution, the Constitution of 1814 . In this period, Norwegian, romantic national feeling flourished, and the Norwegians tried to develop and establish their own national self-worth. The union with Sweden was broken in 1905 after it had been threatened with war, and Norway became an independent kingdom with its own monarch, Haakon VII .
Norway remained neutral during the First World War , and at the outbreak of the Second World War, Norway again declared itself neutral, but was invaded by National Socialist Germany on 9 April 1940 .
Norway became a member of the Western defense alliance NATO in 1949 . Two attempts to join the EU were voted down in referendums by small margins in 1972 and 1994 . Norway has been a close ally of the United States in the post-war period. Large discoveries of oil and natural gas in the North Sea at the end of the 1960s led to tremendous economic growth in the country, which is still ongoing. Traditional industries such as fishing are also part of Norway's economy.
Stone Age (before 1700 BC)
When most of the ice disappeared, vegetation spread over the landscape and due to a warm climate around 2000-3000 BC. the forest grew much taller than in modern times. Land uplift after the ice age led to a number of fjords becoming lakes and dry land. The first people probably came from the south along the coast of the Kattegat and overland into Finnmark from the east. The first people probably lived by gathering, hunting and trapping. A good number of Stone Age settlements have been found which show that such hunting and trapping people stayed for a long time in the same place or returned to the same place regularly. Large amounts of gnawed bones show that they lived on, among other things, reindeer, elk, small game and fish.
Flintstone was imported from Denmark and apart from small natural deposits along the southern coast, all flintstone in Norway is transported by people. At Espevær, greenstone was quarried for tools in the Stone Age, and greenstone tools from Espevær have been found over large parts of Western Norway. Around 2000-3000 BC the usual farm animals such as cows and sheep were introduced to Norway. Livestock probably meant a fundamental change in society in that part of the people had to be permanent residents or live a semi-nomadic life. Livestock farming may also have led to conflict with hunters.
The oldest traces of people in what is today Norway have been found at Pauler , a farm in Brunlanes in Larvik municipality in Vestfold . In 2007 and 2008, the farm has given its name to a number of Stone Age settlements that have been excavated and examined by archaeologists from the Cultural History Museum at UiO. The investigations have been carried out in connection with the new route for the E18 motorway west of Farris. The oldest settlement, located more than 127 m above sea level, is dated to be about 10,400 years old (uncalibrated, more than 11,000 years in real calendar years). From here, the ice sheet was perhaps visible when people settled here. This locality has been named Pauler I, and is today considered to be the oldest confirmed human traces in Norway to date. The place is in the mountains above the Pauler tunnel on the E18 between Larvik and Porsgrunn . The pioneer settlement is a term archaeologists have adopted for the oldest settlement. The archaeologists have speculated about where they came from, the first people in what is today Norway. It has been suggested that they could come by boat or perhaps across the ice from Doggerland or the North Sea, but there is now a large consensus that they came north along what is today the Bohuslän coast. The Fosna culture , the Komsa culture and the Nøstvet culture are the traditional terms for hunting cultures from the Stone Age. One thing is certain - getting to the water was something they mastered, the first people in our country. Therefore, within a short time they were able to use our entire long coast.
In the New Stone Age (4000 BC–1700 BC) there is a theory that a new people immigrated to the country, the so-called Stone Ax People . Rock carvings from this period show motifs from hunting and fishing , which were still important industries. From this period, a megalithic tomb has been found in Østfold .
It is uncertain whether there were organized societies or state-like associations in the Stone Age in Norway. Findings from settlements indicate that many lived together and that this was probably more than one family so that it was a slightly larger, organized herd.
Finnmark
In prehistoric times, animal husbandry and agriculture were of little economic importance in Finnmark. Livelihoods in Finnmark were mainly based on fish, gathering, hunting and trapping, and eventually domestic reindeer herding became widespread in the Middle Ages. Archaeological finds from the Stone Age have been referred to as the Komsa culture and comprise around 5,000 years of settlement. Finnmark probably got its first settlement around 8000 BC. It is believed that the coastal areas became ice-free 11,000 years BC and the fjord areas around 9,000 years BC. after which willows, grass, heather, birch and pine came into being. Finnmarksvidda was covered by pine forest around 6000 BC. After the Ice Age, the land rose around 80 meters in the inner fjord areas (Alta, Tana, Varanger). Due to ice melting in the polar region, the sea rose in the period 6400–3800 BC. and in areas with little land elevation, some settlements from the first part of the Stone Age were flooded. On Sørøya, the net sea level rise was 12 to 14 meters and many residential areas were flooded.
According to Bjørnar Olsen , there are many indications of a connection between the oldest settlement in Western Norway (the " Fosnakulturen ") and that in Finnmark, but it is uncertain in which direction the settlement took place. In the earliest part of the Stone Age, settlement in Finnmark was probably concentrated in the coastal areas, and these only reflected a lifestyle with great mobility and no permanent dwellings. The inner regions, such as Pasvik, were probably used seasonally. The archaeologically proven settlements from the Stone Age in inner Finnmark and Troms are linked to lakes and large watercourses. The oldest petroglyphs in Alta are usually dated to 4200 BC, that is, the Neolithic . Bjørnar Olsen believes that the oldest can be up to 2,000 years older than this.
From around 4000 BC a slow deforestation of Finnmark began and around 1800 BC the vegetation distribution was roughly the same as in modern times. The change in vegetation may have increased the distance between the reindeer's summer and winter grazing. The uplift continued slowly from around 4000 BC. at the same time as sea level rise stopped.
According to Gutorm Gjessing, the settlement in Finnmark and large parts of northern Norway in the Neolithic was semi-nomadic with movement between four seasonal settlements (following the pattern of life in Sami siida in historical times): On the outer coast in summer (fishing and seal catching) and inland in winter (hunting for reindeer, elk and bear). Povl Simonsen believed instead that the winter residence was in the inner fjord area in a village-like sod house settlement. Bjørnar Olsen believes that at the end of the Stone Age there was a relatively settled population along the coast, while inland there was less settlement and a more mobile lifestyle.
Bronze Age (1700 BC–500 BC)
Bronze was used for tools in Norway from around 1500 BC. Bronze is a mixture of tin and copper , and these metals were introduced because they were not mined in the country at the time. Bronze is believed to have been a relatively expensive material. The Bronze Age in Norway can be divided into two phases:
Early Bronze Age (1700–1100 BC)
Younger Bronze Age (1100–500 BC)
For the prehistoric (unwritten) era, there is limited knowledge about social conditions and possible state formations. From the Bronze Age, there are large burial mounds of stone piles along the coast of Vestfold and Agder, among others. It is likely that only chieftains or other great men could erect such grave monuments and there was probably some form of organized society linked to these. In the Bronze Age, society was more organized and stratified than in the Stone Age. Then a rich class of chieftains emerged who had close connections with southern Scandinavia. The settlements became more permanent and people adopted horses and ard . They acquired bronze status symbols, lived in longhouses and people were buried in large burial mounds . Petroglyphs from the Bronze Age indicate that humans practiced solar cultivation.
Finnmark
In the last millennium BC the climate became cooler and the pine forest disappears from the coast; pine forests, for example, were only found in the innermost part of the Altafjord, while the outer coast was almost treeless. Around the year 0, the limit for birch forest was south of Kirkenes. Animals with forest habitats (elk, bear and beaver) disappeared and the reindeer probably established their annual migration routes sometime at that time. In the period 1800–900 BC there were significantly more settlements in and utilization of the hinterland was particularly noticeable on Finnmarksvidda. From around 1800 BC until year 0 there was a significant increase in contact between Finnmark and areas in the east including Karelia (where metals were produced including copper) and central and eastern Russia. The youngest petroglyphs in Alta show far more boats than the earlier phases and the boats are reminiscent of types depicted in petroglyphs in southern Scandinavia. It is unclear what influence southern Scandinavian societies had as far north as Alta before the year 0. Many of the cultural features that are considered typical Sami in modern times were created or consolidated in the last millennium BC, this applies, among other things, to the custom of burying in brick chambers in stone urns. The Mortensnes burial ground may have been used for 2000 years until around 1600 AD.
Iron Age (c. 500 BC–c. 1050 AD)
The Einangsteinen is one of the oldest Norwegian runestones; it is from the 4th century
Simultaneous production of Vikings
Around 500 years BC the researchers reckon that the Bronze Age will be replaced by the Iron Age as iron takes over as the most important material for weapons and tools. Bronze, wood and stone were still used. Iron was cheaper than bronze, easier to work than flint , and could be used for many purposes; iron probably became common property. Iron could, among other things, be used to make solid and sharp axes which made it much easier to fell trees. In the Iron Age, gold and silver were also used partly for decoration and partly as means of payment. It is unknown which language was used in Norway before our era. From around the year 0 until around the year 800, everyone in Scandinavia (except the Sami) spoke Old Norse , a North Germanic language. Subsequently, several different languages developed in this area that were only partially mutually intelligible. The Iron Age is divided into several periods:
Early Iron Age
Pre-Roman Iron Age (c. 500 BC–c. 0)
Roman Iron Age (c. 0–c. AD 400)
Migration period (approx. 400–600). In the migration period (approx. 400–600), new peoples came to Norway, and ruins of fortress buildings etc. are interpreted as signs that there has been talk of a violent invasion.
Younger Iron Age
Merovingian period (500–800)
The Viking Age (793–1066)
Norwegian Vikings go on plundering expeditions and trade voyages around the coastal countries of Western Europe . Large groups of Norwegians emigrate to the British Isles , Iceland and Greenland . Harald Hårfagre starts a unification process of Norway late in the 8th century , which was completed by Harald Hardråde in the 1060s . The country was Christianized under the kings Olav Tryggvason , fell in the battle of Svolder ( 1000 ) and Olav Haraldsson (the saint), fell in the battle of Stiklestad in 1030 .
Sources of prehistoric times
Shrinking glaciers in the high mountains, including in Jotunheimen and Breheimen , have from around the year 2000 uncovered objects from the Viking Age and earlier. These are objects of organic material that have been preserved by the ice and that elsewhere in nature are broken down in a few months. The finds are getting older as the melting makes the archaeologists go deeper into the ice. About half of all archaeological discoveries on glaciers in the world are made in Oppland . In 2013, a 3,400-year-old shoe and a robe from the year 300 were found. Finds at Lomseggen in Lom published in 2020 revealed, among other things, well-preserved horseshoes used on a mountain pass. Many hundreds of items include preserved clothing, knives, whisks, mittens, leather shoes, wooden chests and horse equipment. A piece of cloth dated to the year 1000 has preserved its original colour. In 2014, a wooden ski from around the year 700 was found in Reinheimen . The ski is 172 cm long and 14 cm wide, with preserved binding of leather and wicker.
Pytheas from Massalia is the oldest known account of what was probably the coast of Norway, perhaps somewhere on the coast of Møre. Pytheas visited Britannia around 325 BC. and traveled further north to a country by the "Ice Sea". Pytheas described the short summer night and the midnight sun farther north. He wrote, among other things, that people there made a drink from grain and honey. Caesar wrote in his work about the Gallic campaign about the Germanic tribe Haruders. Other Roman sources around the year 0 mention the land of the Cimbri (Jutland) and the Cimbri headlands ( Skagen ) and that the sources stated that Cimbri and Charyds lived in this area. Some of these peoples may have immigrated to Norway and there become known as hordes (as in Hordaland). Sources from the Mediterranean area referred to the islands of Scandia, Scandinavia and Thule ("the outermost of all islands"). The Roman historian Tacitus wrote around the year 100 a work about Germania and mentioned the people of Scandia, the Sviones. Ptolemy wrote around the year 150 that the Kharudes (Hordes) lived further north than all the Cimbri, in the north lived the Finnoi (Finns or Sami) and in the south the Gutai (Goths). The Nordic countries and Norway were outside the Roman Empire , which dominated Europe at the time. The Gothic-born historian Jordanes wrote in the 5th century about 13 tribes or people groups in Norway, including raumaricii (probably Romerike ), ragnaricii ( Ranrike ) and finni or skretefinni (skrid finner or ski finner, i.e. Sami) as well as a number of unclear groups. Prokopios wrote at the same time about Thule north of the land of the Danes and Slavs, Thule was ten times as big as Britannia and the largest of all the islands. In Thule, the sun was up 40 days straight in the summer. After the migration period , southern Europeans' accounts of northern Europe became fuller and more reliable.
Settlement in prehistoric times
Norway has around 50,000 farms with their own names. Farm names have persisted for a long time, over 1000 years, perhaps as much as 2000 years. The name researchers have arranged different types of farm names chronologically, which provides a basis for determining when the place was used by people or received a permanent settlement. Uncompounded landscape names such as Haug, Eid, Vik and Berg are believed to be the oldest. Archaeological traces indicate that some areas have been inhabited earlier than assumed from the farm name. Burial mounds also indicate permanent settlement. For example, the burial ground at Svartelva in Løten was used from around the year 0 to the year 1000 when Christianity took over. The first farmers probably used large areas for inland and outland, and new farms were probably established based on some "mother farms". Names such as By (or Bø) show that it is an old place of residence. From the older Iron Age, names with -heim (a common Germanic word meaning place of residence) and -stad tell of settlement, while -vin and -land tell of the use of the place. Farm names in -heim are often found as -um , -eim or -em as in Lerum and Seim, there are often large farms in the center of the village. New farm names with -city and -country were also established in the Viking Age . The first farmers probably used the best areas. The largest burial grounds, the oldest archaeological finds and the oldest farm names are found where the arable land is richest and most spacious.
It is unclear whether the settlement expansion in Roman times, migrations and the Iron Age is due to immigration or internal development and population growth. Among other things, it is difficult to demonstrate where in Europe the immigrants have come from. The permanent residents had both fields (where grain was grown) and livestock that grazed in the open fields, but it is uncertain which of these was more important. Population growth from around the year 200 led to more utilization of open land, for example in the form of settlements in the mountains. During the migration period, it also seems that in parts of the country it became common to have cluster gardens or a form of village settlement.
Norwegian expansion northwards
From around the year 200, there was a certain migration by sea from Rogaland and Hordaland to Nordland and Sør-Troms. Those who moved settled down as a settled Iron Age population and became dominant over the original population which may have been Sami . The immigrant Norwegians, Bumen , farmed with livestock that were fed inside in the winter as well as some grain cultivation and fishing. The northern border of the Norwegians' settlement was originally at the Toppsundet near Harstad and around the year 500 there was a Norwegian settlement to Malangsgapet. That was as far north as it was possible to grow grain at the time. Malangen was considered the border between Hålogaland and Finnmork until around 1400 . Further into the Viking Age and the Middle Ages, there was immigration and settlement of Norwegian speakers along the coast north of Malangen. Around the year 800, Norwegians lived along the entire outer coast to Vannøy . The Norwegians partly copied Sami livelihoods such as whaling, fur hunting and reindeer husbandry. It was probably this area between Malangen and Vannøy that was Ottar from the Hålogaland area. In the Viking Age, there were also some Norwegian settlements further north and east. East of the North Cape are the scattered archaeological finds of Norwegian settlement in the Viking Age. There are Norwegian names for fjords and islands from the Viking Age, including fjord names with "-anger". Around the year 1050, there were Norwegian settlements on the outer coast of Western Finnmark. Traders and tax collectors traveled even further.
North of Malangen there were Norse farming settlements in the Iron Age. Malangen was considered Finnmark's western border until 1300. There are some archaeological traces of Norse activity around the coast from Tromsø to Kirkenes in the Viking Age. Around Tromsø, the research indicates a Norse/Sami mixed culture on the coast.
From the year 1100 and the next 200–300 years, there are no traces of Norwegian settlement north and east of Tromsø. It is uncertain whether this is due to depopulation, whether it is because the Norwegians further north were not Christianized or because there were no churches north of Lenvik or Tromsø . Norwegian settlement in the far north appears from sources from the 14th century. In the Hanseatic period , the settlement was developed into large areas specialized in commercial fishing, while earlier (in the Viking Age) there had been farms with a combination of fishing and agriculture. In 1307 , a fortress and the first church east of Tromsø were built in Vardø . Vardø became a small Norwegian town, while Vadsø remained Sami. Norwegian settlements and churches appeared along the outermost coast in the Middle Ages. After the Reformation, perhaps as a result of a decline in fish stocks or fish prices, there were Norwegian settlements in the inner fjord areas such as Lebesby in Laksefjord. Some fishing villages at the far end of the coast were abandoned for good. In the interior of Finnmark, there was no national border for a long time and Kautokeino and Karasjok were joint Norwegian-Swedish areas with strong Swedish influence. The border with Finland was established in 1751 and with Russia in 1826.
On a Swedish map from 1626, Norway's border is indicated at Malangen, while Sweden with this map showed a desire to control the Sami area which had been a common area.
The term Northern Norway only came into use at the end of the 19th century and administratively the area was referred to as Tromsø Diocese when Tromsø became a bishopric in 1840. There had been different designations previously: Hålogaland originally included only Helgeland and when Norse settlement spread north in the Viking Age and the Middle Ages, Hålogaland was used for the area north approximately to Malangen , while Finnmark or "Finnmarken", "the land of the Sami", lay outside. The term Northern Norway was coined at a cafe table in Kristiania in 1884 by members of the Nordlændingernes Forening and was first commonly used in the interwar period as it eventually supplanted "Hålogaland".
State formation
The battle in Hafrsfjord in the year 872 has long been regarded as the day when Norway became a kingdom. The year of the battle is uncertain (may have been 10-20 years later). The whole of Norway was not united in that battle: the process had begun earlier and continued a couple of hundred years later. This means that the geographical area became subject to a political authority and became a political unit. The geographical area was perceived as an area as it is known, among other things, from Ottar from Hålogaland's account for King Alfred of Wessex around the year 880. Ottar described "the land of the Norwegians" as very long and narrow, and it was narrowest in the far north. East of the wasteland in the south lay Sveoland and in the north lay Kvenaland in the east. When Ottar sailed south along the land from his home ( Malangen ) to Skiringssal, he always had Norway ("Nordveg") on his port side and the British Isles on his starboard side. The journey took a good month. Ottar perceived "Nordveg" as a geographical unit, but did not imply that it was a political unit. Ottar separated Norwegians from Swedes and Danes. It is unclear why Ottar perceived the population spread over such a large area as a whole. It is unclear whether Norway as a geographical term or Norwegians as the name of a ethnic group is the oldest. The Norwegians had a common language which in the centuries before Ottar did not differ much from the language of Denmark and Sweden.
According to Sverre Steen, it is unlikely that Harald Hårfagre was able to control this entire area as one kingdom. The saga of Harald was written 300 years later and at his death Norway was several smaller kingdoms. Harald probably controlled a larger area than anyone before him and at most Harald's kingdom probably included the coast from Trøndelag to Agder and Vestfold as well as parts of Viken . There were probably several smaller kingdoms of varying extent before Harald and some of these are reflected in traditional landscape names such as Ranrike and Ringerike . Landscape names of "-land" (Rogaland) and "-mark" (Hedmark) as well as names such as Agder and Sogn may have been political units before Harald.
According to Sverre Steen
Water, saturated with dissoluted Calciumhydrogencarbonate forms dripstones. Drop for drop a little quanitity of calcite (or aragonite) is left (when carbondioxide vanishes in the air of the cave) and accumulates to a dripstone.
Former military training ground Scharpenacken, Wuppertal
Ehemaliger Truppenübungsplatz Scharpenacken, Wuppertal
"Ridgely's Delight is an historic residential neighborhood in Baltimore, Maryland, United States. Its borders are formed by Russell and Greene Streets to the east, West Pratt Street to the north, and Martin Luther King Jr. Boulevard from the western to southern tips. It is adjacent to the University of Maryland, Baltimore, Oriole Park at Camden Yards, and M&T Bank Stadium. It is situated a short walk from MARC Train and the Light Rail's Camden Station, which has made it a popular residence of Washington, D.C. and suburban Baltimore commuters. It is within a 5-minute walk of both Oriole Park at Camden Yards and M&T Bank Stadium and a 10-minute walk from Baltimore's historic Inner Harbor.
The land tract of Ridgley's Delight was surveyed in 1732 for Charles Ridgley.
In 1792, James McHenry purchased a 95-acre (38 ha) tract from Ridgely's Delight and named it Fayetteville in honor of his friend Lafayette.
With its name derived from Charles Ridgely II's plantation Ridgely's Whim, Ridgely's Delight was originally inhabited by craftspeople but later became home to affluent professionals who used their resources to make the rowhouses more ornate.
Ridgely's Delight is the birthplace of Babe Ruth and home to the Babe Ruth Birthplace Museum on Emory Street. Several bars and shops are located in the neighborhood, most popularly Quigley's Half-Irish Pub, Camden Pub, Corner Bistro & Wine Bar, and Peace and a Cup of Joe.
Baltimore (/ˈbɔːltɪmɔːr/ BAWL-tim-or, locally: /bɔːldəˈmɔːr/ bawl-da-MOR or /ˈbɔːlmər/ BAWL-mər) is the most populous city in the U.S. state of Maryland, fourth most populous city in the Mid-Atlantic, and the 30th most populous city in the United States with a population of 585,708 in 2020. Baltimore was designated an independent city by the Constitution of Maryland in 1851, and today is the most populous independent city in the United States. As of 2021, the population of the Baltimore metropolitan area was estimated to be 2,838,327, making it the 20th largest metropolitan area in the country. Baltimore is located about 40 miles (64 km) north northeast of Washington, D.C., making it a principal city in the Washington–Baltimore combined statistical area (CSA), the third-largest CSA in the nation, with a 2021 estimated population of 9,946,526.
Prior to European colonization, the Baltimore region was used as hunting grounds by the Susquehannock Native Americans, who were primarily settled further northwest than where the city was later built. Colonists from the Province of Maryland established the Port of Baltimore in 1706 to support the tobacco trade with Europe, and established the Town of Baltimore in 1729. The first printing press and newspapers were introduced to Baltimore by Nicholas Hasselbach and William Goddard respectively, in the mid-18th century.
The Battle of Baltimore was a pivotal engagement during the War of 1812, culminating in the failed British bombardment of Fort McHenry, during which Francis Scott Key wrote a poem that would become "The Star-Spangled Banner", which was eventually designated as the American national anthem in 1931. During the Pratt Street Riot of 1861, the city was the site of some of the earliest violence associated with the American Civil War.
The Baltimore and Ohio Railroad, the oldest railroad in the United States, was built in 1830 and cemented Baltimore's status as a major transportation hub, giving producers in the Midwest and Appalachia access to the city's port. Baltimore's Inner Harbor was once the second leading port of entry for immigrants to the United States. In addition, Baltimore was a major manufacturing center. After a decline in major manufacturing, heavy industry, and restructuring of the rail industry, Baltimore has shifted to a service-oriented economy. Johns Hopkins Hospital and Johns Hopkins University are the city's top two employers. Baltimore and its surrounding region are home to the headquarters of a number of major organizations and government agencies, including the NAACP, ABET, the National Federation of the Blind, Catholic Relief Services, the Annie E. Casey Foundation, World Relief, the Centers for Medicare & Medicaid Services, and the Social Security Administration. Baltimore is also home to the Baltimore Orioles of Major League Baseball and the Baltimore Ravens of the National Football League.
Many of Baltimore's neighborhoods have rich histories. The city is home to some of the earliest National Register Historic Districts in the nation, including Fell's Point, Federal Hill, and Mount Vernon. These were added to the National Register between 1969 and 1971, soon after historic preservation legislation was passed. Baltimore has more public statues and monuments per capita than any other city in the country. Nearly one third of the city's buildings (over 65,000) are designated as historic in the National Register, which is more than any other U.S. city. Baltimore has 66 National Register Historic Districts and 33 local historic districts. The historical records of the government of Baltimore are located at the Baltimore City Archives." - info from Wikipedia.
The fall of 2022 I did my 3rd major cycling tour. I began my adventure in Montreal, Canada and finished in Savannah, GA. This tour took me through the oldest parts of Quebec and the 13 original US states. During this adventure I cycled 7,126 km over the course of 2.5 months and took more than 68,000 photos. As with my previous tours, a major focus was to photograph historic architecture.
Now on Instagram.
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Just playing with brushes and ideas for new images, in low res.
Thanks to Tempo, for his fetus model image.
danish radio concert hall, copenhagen, denmark 2002-2009.
architects: atelier jean nouvel.
studio 1, the main concert hall.
admirers of german architect hans scharoun and his work to reinvent the building typologies of prewar europe in the form of meaningful, democratic institutions and monuments will recognize his berlin philharmonic concert hall as the model for nouvel's copenhagen space. scharoun broke down the concert hall into terraces of seating surrounding the stage, each of them about the size of the stage, so as to dismantle the classical configuration of audience and orchestra as opposing sides.
I suspect there are sound values behind many of the strangest of nouvel's choices and here, for once, they become obvious.
the upper part of the room, however, remains a mystery to me: gypsum board curves painted in a stretched version of the evening sky from edvard munch's the scream, like some bad highschool photoshop project. I prefer munch's late paintings but mostly for not being the early ones. why I should be confronted with memories of the scream when going to a concert eludes me.
but a kind of pattern arises, telling us of nouvel's method, and it is confirmed when viewing the main concert hall from the outside where it is shaped as a meteor - its glowing lava interior shown here. the idea for the shape apparently came from reading that awful, danish novel, "miss smilla's sense of snow", whose central characters all hunt for a meteorite embedded in a glacier on greenland.
why this image should carry any significance in connection with a national radio concert hall is never explained and I doubt it ever will be. what we are looking at is a postmodern architect shooting from the hip. he believes in seduction and cinematic moments, he believes in storytelling and in tying a building to local culture. but the grand piano studio with a grand piano, the modern-architecture-as-scaffolding, the ceiling as the sky from munch's scream, and the concert hall as a meteorite from smilla, these images never come together because they are not connected except as popular culture's understanding of what higher culture must be.
ultimately, nouvel doing free associations on nordic culture is incoherent - he is giving us the architectural equivalent of a mixed metaphor and the necessary synthesis never occurs. that the building has obvious functional qualities and good acoustics is not enough exactly because it is so insistent on its own rambling imagery.
more words, yada, yada, yada.
{Wearing} Dress thanks to ModCloth (available in sizes XS-2X) / Bangle from India / Earrings thanks to ByBoe / BCBG Bag / Nine West Peep Toes
Formed in 1969 by the amalgamation of the
Royal Horse Guards formed 1650 and
The Royal Dragoons formed1661. Both were part of Oliver Cromwell's New Model Army.
The helmet is 1871 pattern and is 17 inches high.
ln its center is an 8 pointed Guards Star with the cross of St George and garter in red and blue enamel.
The inscription on the badge says
Honi Soit Qui Mal y Pense which means
Evil Be To Those That Evil Thinks.
This is an officers helmet and can be seen around Whitehall in London.
This is part of my private collection
Henry Moore - Form and Material - Museum Beelden aan Zee - The Hague
In collaboration with the Henry Moore Foundation, Museum Beelden aan Zee has made a selection of works from the artist's substantial oeuvre. Around 70 objects and sculptures portray the artistic vision and creative process of one of the most important innovators of modern sculpture. The exhibition in Beelden aan Zee focuses on the influence of nature on his work and his growth and development as a sculptor. From promoting direct carving – carving without using preparatory sketches and studies – to experimenting with casting in lead and bronze. Henry Moore (1898-1986) is one of the most important British artists of the twentieth century. His sculptures balance on the boundary between figurative and abstract art and continue to be a source of inspiration to artists. His work has a recognisable and characteristic formal language. Important themes in his oeuvre are ‘mother and child’ and his reclining figures, which he explored extensively.
From the 1920s, Moore participated in countless British and international exhibitions, with solo as well as group exhibitions, he sold work on a regular basis, and so made a name for himself as an important modernist sculptor. However, the Second World War called a halt to these positive developments. Henry Moore left his teaching post and took up a commission as a war artist. It was in this capacity that he produced his deeply moving Shelter Drawings of Londoners crowding the city's underground stations sheltering from the Blitz. In the 1950s he created larger groups of figures. The prices for his works increased considerably and his fame as an international artist continued to grow. In later years he served as a trustee at both the Tate Gallery and the National Gallery and he was the recipient of a large number of prizes and honours.