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Lake Sary-Chelek
Sary-Chelek (also Sarychelek, Kyrgyz: Сарычелек) is a mountain lake located in Sary-Chelek Nature Reserve in Jalal-Abad Province in Western Kyrgyzstan. It is north of Arkyt (the park headquarters) at the eastern end of the Chatkal Range. There are a number of smaller lakes in the area. The lake is long and its average width is . Its area is and its maximum depth is . It is drained by the river Toskool, a tributary of the Kojata King Kojata or The Unlooked for Prince or Prince Unexpected (Polish: ''O królewiczu Niespodzianku'') is a Slavonic fairy tale, of Polish origin. Louis Léger remarked that its source (''Bajarz polski'') was "one of the most important collections of .... References External linksSary-Chelek Nature Reserve - Photogalleryby Azamat Imanaliev Sary-Chelek Sary-Chelek Biosphere reserves of Kyrgyzstan {{JalalAbad-geo-stub ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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Kojata (river)
The Kojata ( ky, Кожата) is a right tributary of the Kara-Suu in Jalal-Abad Region, Kyrgyzstan. Its source is in the Chatkal Range, western Tian Shan mountains, and is fed by the Toskool, which flows out of Lake Sary-Chelek Sary-Chelek (also Sarychelek, Kyrgyz: Сарычелек) is a mountain lake located in Sary-Chelek Nature Reserve in Jalal-Abad Province in Western Kyrgyzstan. It is north of Arkyt (the park headquarters) at the eastern end of the Chatkal Range. .... It is 18 km long and has a drainage basin of 280 km2. It discharges into the Kara-Suu near Kyzyl-Tuu.Soviet military maK-43-19(1:200,000) References Rivers of Kyrgyzstan {{JalalAbad-geo-stub ...
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Kyrgyzstan
Kyrgyzstan,, pronounced or the Kyrgyz Republic, is a landlocked country in Central Asia. Kyrgyzstan is bordered by Kazakhstan to the north, Uzbekistan to the west, Tajikistan to the south, and the People's Republic of China to the east. Its capital and largest city is Bishkek. Ethnic Kyrgyz make up the majority of the country's seven million people, followed by significant minorities of Uzbeks and Russians. The Kyrgyz language is closely related to other Turkic languages. Kyrgyzstan's history spans a variety of cultures and empires. Although geographically isolated by its highly mountainous terrain, Kyrgyzstan has been at the crossroads of several great civilizations as part of the Silk Road along with other commercial routes. Inhabited by a succession of tribes and clans, Kyrgyzstan has periodically fallen under larger domination. Turkic nomads, who trace their ancestry to many Turkic states. It was first established as the Yenisei Kyrgyz Khaganate later in the ...
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Kyrgyz Language
Kyrgyz (; autonym: , tr. ''Kyrgyz tili'', ) is a Turkic language of the Kipchak branch spoken in Central Asia. Kyrgyz is the official language of Kyrgyzstan and a significant minority language in the Kizilsu Kyrgyz Autonomous Prefecture in Xinjiang, China and in the Gorno-Badakhshan Autonomous Region of Tajikistan. There is a very high level of mutual intelligibility between Kyrgyz, Kazakh, and Altay. A dialect of Kyrgyz known as Pamiri Kyrgyz is spoken in Afghanistan and Pakistan. Kyrgyz is also spoken by many ethnic Kyrgyz through the former Soviet Union, Afghanistan, Turkey, parts of northern Pakistan, and Russia. Kyrgyz was originally written in Göktürk script, gradually replaced by the Perso-Arabic alphabet (in use until 1928 in the USSR, still in use in China). Between 1928 and 1940 a Latin-script alphabet, the Uniform Turkic Alphabet, was used. In 1940, Soviet authorities replaced the Latin script with the Cyrillic alphabet for all Turkic countries. When Kyrgy ...
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Sary-Chelek Nature Reserve
The Sary-Chelek Nature Reserve ( ky, Сары-Челек мамлекеттик коругу, russian: Сары-Челекский государственный заповедник) is located in Aksy District, Jalal-Abad Region in western Kyrgyzstan. Established in 1959, it currently covers 23,868 hectares. In 1978 it was designated as a World Biosphere reserve by UNESCO. The Reserve is located at altitudes from above sea level. The name of Sary Chelek translates as "Yellow bucket" from Kyrgyz language. Geography Sary-Chelek Nature Reserve is approximately to the northwest of Tash-Kömür town. The reserve currently occupies , including s core area, and transition area. Its headquarters are in the village Arkyt. Description The comparatively large Lake Sary-Chelek is the main feature of the nature reserve. In the low hills south of Lake Sary-Chelek there are 6 smaller lakes: Kylaaköl, Iyriköl, Bakalyköl, Aramköl, Chöychökköl, and Chachaköl. The river Kojata King K ...
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Jalal-Abad Province
Jalal-Abad Region ( ky, Жалал-Абад облусу, Jalal-Abad oblusu; russian: Джалал-Абадская область, Dzhalal-Abadskaya oblast) is a region (''oblast'') of Kyrgyzstan. Its capital is the city of the same name, Jalal-Abad. It is surrounded by (clockwise from the north) Talas Region, Chüy Region, Naryn Region, Osh Region, and Uzbekistan. Jalal-Abad Region was established on 21 November 1939. On 27 January 1959 it became a part of Osh Region, but regained its old status as a region on 14 December 1990. Its total area is . The resident population of the region was 1,260,617 as of January 2021. The region has a sizeable Uzbek (24.8% in 2009) minority. Geography Jalal-Abad Region covers (16.2% of total country's area) in central-western Kyrgyzstan. The southern edge of the region is part of the Ferghana Valley. The rest of the region is mountainous. M41, the main north-south highway from Bishkek to Osh, takes a very crooked route down the center of t ...
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Arkyt, Kyrgyzstan
Arkyt ( ky, Аркыт, uz, Arkit) is a village in Jalal-Abad Region of Kyrgyzstan, located south of Lake Sary-Chelek and north of Kerben. It is part of the Aksy District. It is the headquarters of the Sary-Chelek Nature Reserve The Sary-Chelek Nature Reserve ( ky, Сары-Челек мамлекеттик коругу, russian: Сары-Челекский государственный заповедник) is located in Aksy District, Jalal-Abad Region in western Kyrgy .... Its population was 1,379 in 2021. References Populated places in Jalal-Abad Region {{JalalAbad-geo-stub ...
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Lakes Of Kyrgyzstan
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Mountain Lakes
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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