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Jigme Singye Wangchuck National Park
Jigme Singye Wangchuck National Park (formerly Black Mountains National Park) covers an area of in central Bhutan. It protects a large area of the Black Mountains, a sub−range of the Himalayan Range System. The park occupies most of the Trongsa District, as well as parts of: Sarpang, Tsirang, Wangdue Phodrang, and Zhemgang Districts. The park is bound to the east by the Mangde Chhu, and reaches the Sankosh River−Punatsangchu basin to the west. Jigme Singye abuts Royal Manas National Park to the southeast. Along the border of the park from the north to the southeast run Bhutan's main east-west and north-south highways. It is also connected via biological corridors to other national parks in northern, eastern, central, and southern Bhutan. Habitats of the Eastern Himalayan broadleaf forests ecoregion are protected within the park Geography Jigme Singye Wangchuck National Park is the most centrally located among the national parks of Bhutan. Covering over an area of 1730&n ...
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Sarpang District
Sarpang District (Dzongkha: གསར་སྤང་རྫོང་ཁག་; Wylie: ''Gsar-spang rdzong-khag''; also known as "Geylegphug") is one of the 20 dzongkhags (districts) comprising Bhutan. Sarpang covers a total area of 1,946 sq km and stretches from Lhamoizhingkha in West Bhutan to Manas National Park in the east. Sarpang Dzongkhag is divided into one dungkhag, Gelephu, and 12 gewogs. Languages The dominant language in Sarpang is Nepali, an Indo-European language spoken by the heterogeneous Lhotshampa community. The East Bodish Kheng language is also spoken in the northeastern reaches of the district. Administrative divisions Sarpang District is currently divided into twelve village blocks (or '' gewogs''): * Chhuzagang Gewog * Chhudzom Gewog * Dekiling Gewog * Gakiling Gewog * Gelephu Gewog * Jigmechhoeling Gewog *Samtenling Gewog * Senghe Gewog * Serzhong Gewog * Shompangkha Gewog * Tareythang Gewog * Umling Gewog Environment Much of Sarpang District consists of ...
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Sarpang
Sarpang, also transliterated as Sarbhang or Sarbang, is a thromde or town in Sarpang District in southern Bhutan Bhutan (; dz, འབྲུག་ཡུལ་, Druk Yul ), officially the Kingdom of Bhutan,), is a landlocked country in South Asia. It is situated in the Eastern Himalayas, between China in the north and India in the south. A mountainous .... References External linksSatellite map at Maplandia.com Populated places in Bhutan {{Bhutan-geo-stub ...
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Athang Gewog
Athang Gewog (Dzongkha: ཨ་ཐང་) is a gewog (village block) of Wangdue Phodrang District, Bhutan Bhutan (; dz, འབྲུག་ཡུལ་, Druk Yul ), officially the Kingdom of Bhutan,), is a landlocked country in South Asia. It is situated in the Eastern Himalayas, between China in the north and India in the south. A mountainous .... Athang Gewog is one of the most remotest Gewogs in Wangdue Phodrang District. Two Chiwogs, namely Lopokha-Phaktakha and Lomtshokha makes up the Athang Gewog and Rukha village is composed of two Chiwongs(Lawa Lamga and Rukha). With the settlements widely scattered, the Gewog covers an estimated area of 746 km2. References Gewogs of Bhutan Wangdue Phodrang District {{coord missing, Bhutan ...
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Mangde Chhu River
Mangde Chhu or Tongsa river flows in central Bhutan traversing roughly north–south. The river rises in Wangdue Phodrang district (or dzongkhag in Dzongkha), near Gangkhar Puensum, Bhutan's highest peak at . Bhutan's main east–west highway crosses the Mangde Chhu about west of Trongsa. South of Trongsa, the river drains the eastern slopes of the Black Mountains (Bhutan), and forms the eastern boundaries of Black Mountain National Park and Royal Manas National Park. Another highway follows the river south from Trongsa to Shemgang. The highway leaves the river at Tingtinbi, and eventually reaches the Indian border at Gelegphug. South of Tingtinbi, the Mangde is joined by the Bumthang River from the east, and is known as the Tongasa. Shortly before entering India in Assam, the Manas River flows into the river from the east, and the river exits Bhutan near Manas. Important towns and areas through which the Trongsa - Gelegphug road passes are Shemgang (Shamgong), Taama, Bat ...
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Headwaters
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest t ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Temperate Forest
A temperate forest is a forest found between the tropical and boreal regions, located in the temperate zone. It is the second largest biome on our planet, covering 25% of the world's forest area, only behind the boreal forest, which covers about 33%. These forests cover both hemispheres at latitudes ranging from 25 to 50 degrees, wrapping the planet in a belt similar to that of the boreal forest. Due to its large size spanning several continents, there are several main types: deciduous, coniferous, mixed forest, and rainforest. Climate The climate of a temperate forest is highly variable depending on the location of the forest. For example, Los Angeles and Vancouver, Canada are both considered to be located in a temperate zone, however, Vancouver is located in a temperate rainforest, while Los Angeles is more subtropical. Temperate forests typically have winters that often reach below freezing, however even this is not always true. The East Coast forests retain their deciduous n ...
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Biodiversity
Biodiversity or biological diversity is the variety and variability of life on Earth. Biodiversity is a measure of variation at the genetic (''genetic variability''), species (''species diversity''), and ecosystem (''ecosystem diversity'') level. Biodiversity is not distributed evenly on Earth; it is usually greater in the tropics as a result of the warm climate and high primary productivity in the region near the equator. Tropical forest ecosystems cover less than 10% of earth's surface and contain about 90% of the world's species. Marine biodiversity is usually higher along coasts in the Western Pacific, where sea surface temperature is highest, and in the mid-latitudinal band in all oceans. There are latitudinal gradients in species diversity. Biodiversity generally tends to cluster in hotspots, and has been increasing through time, but will be likely to slow in the future as a primary result of deforestation. It encompasses the evolutionary, ecological, and cultural ...
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Migratory Bird
Bird migration is the regular seasonal movement, often north and south along a flyway, between Breeding in the wild, breeding and wintering grounds. Many species of bird migrate. Animal migration, Migration carries high costs in predation and mortality, including from hunting by humans, and is driven primarily by the availability of food. It occurs mainly in the northern hemisphere, where birds are funneled onto specific routes by natural barriers such as the Mediterranean Sea or the Caribbean Sea. Migration of species such as storks, European turtle dove, turtle doves, and swallows was recorded as many as 3,000 years ago by Ancient Greece, Ancient Greek authors, including Homer and Aristotle, and in the Book of Job. More recently, Johannes Leche began recording dates of arrivals of spring migrants in Finland in 1749, and modern scientific studies have used techniques including bird ringing and Animal migration tracking#Satellite tracking, satellite tracking to trace migrant ...
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Pinus Roxburghii
''Pinus roxburghii'', commonly known as chir pine or longleaf Indian pine, is a species of pine tree native to the Himalayas. It was named after William Roxburgh. Description ''Pinus roxburghii'' is a large tree reaching with a trunk diameter of up to , exceptionally . The bark is red-brown, thick and deeply fissured at the base of the trunk, thinner and flaky in the upper crown. The leaves are needle-like, in fascicles of three, very slender, long, and distinctly yellowish green. The cones are ovoid conic, long and broad at the base when closed, green at first, ripening glossy chestnut-brown when 24 months old. They open slowly over the next year or so, or after being heated by a forest fire, to release the seeds, opening to broad. The seeds are long, with a wing, and are wind- dispersed. Similar species ''Pinus roxburghii'' is closely related to '' P. canariensis'' (Canary Island pine), '' P. brutia'' (Turkish pine) and '' P. pinaster'' (maritime p ...
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Eastern Himalaya
] The Eastern Himalayas extend from eastern Nepal across Northeast India, Bhutan, the Tibet Autonomous Region to Yunnan in China and northern Myanmar. The climate of this region is influenced by the monsoon of South Asia from June to September. It is a biodiversity hotspot, with notable biocultural diversity. Geologic strata The Eastern Himalayas have a much more sophisticated geomorphic history and pervasive topographic features than the Central Himalayas. In the southwest of the Sub-Himalayan Range, Sub-Himalayas lies the Singalila Ridge, the western end of a group of uplands in Nepal. Most of the Sub-Himalayas are in Nepal; a small portion reaches into Sikkim, India and a fragment is in the southern half of Bhutan. The region's topography, in part, has facilitated the region's rich biological diversity and ecosystem structure. The Buxa range of Indo-Bhutan is also a part of the ancient rocks of the Himalayas. The ancient folds, running mainly along an east-west axis, were worn ...
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