Tannu-Ola Mountains
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Tannu-Ola Mountains
The Tannu-Ola mountains ( tyv, Таңды-Уула, ''Tañdı-Uula'', uniturk, Taᶇdь-Uula, – Tangdy-Uula mountains; mn, Тагнын нуруу, ''Tağnîn nurú'', , russian: Танну-Ола, ) is a mountain range in southern Siberia, in the Tuva Republic of Russia. It extends in an east–west direction and curves along the Mongolian border. Its highest peak reaches . The Tannu-ola mountains are mentioned in the 13th-century text ''The Secret History of the Mongols'' under the name "Tanglu mountains" (唐麓), and also in the ''JāmiʿAl-tawārīkh'' of Rashid-al-Din Hamadani (1247–1318) under the name "Toungat mountains" (تنغات). By the Qing dynasty the name has been changed to Tangnu (唐努) mountains, from which the modern name is derived. All names are probably rooted in the old Turkic word ''taŋ'' - "wonder, awe, wondrous." Geography The northern slopes are part of the watershed of the Yenisei River, facing the western Sayan Mountains. The eastern end to ...
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Russia
Russia (, , ), or the Russian Federation, is a List of transcontinental countries, transcontinental country spanning Eastern Europe and North Asia, Northern Asia. It is the List of countries and dependencies by area, largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across Time in Russia, eleven time zones and shares Borders of Russia, land boundaries with fourteen countries, more than List of countries and territories by land borders, any other country but China. It is the List of countries and dependencies by population, world's ninth-most populous country and List of European countries by population, Europe's most populous country, with a population of 146 million people. The country's capital and List of cities and towns in Russia by population, largest city is Moscow, the List of European cities by population within city limits, largest city entirely within E ...
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Sayan Mountains
The Sayan Mountains (russian: Саяны ''Sajany''; mn, Соёны нуруу, ''Soyonï nurû''; otk, 𐰚𐰇𐰏𐰢𐰤, Kögmen) are a mountain range in southern Siberia, Russia (Buryatia, Irkutsk Oblast, Krasnoyarsk Krai, Tuva Republic and Khakassia) and northern Mongolia. In the past, it served as the border between Mongolia and Russia. The Sayan Mountains' towering peaks and cool lakes southwest of Tuva give rise to the tributaries that merge to become one of Siberia's major rivers, the Yenisei River, which flows north over 3,400 kilometres (2000 mi) to the Arctic Ocean. This is a protected and isolated area, having been kept closed by the Soviet Union since 1944. Geography Western Sayan At 92°E the Western Sayan system is pierced by the Ulug-Khem (russian: Улуг-Хем) or Upper Yenisei River, and at 106°, at its eastern extremity, it terminates above the depression of the Selenga-Orkhon Valley. It stretches almost at a right angle to the Western Sayan fo ...
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Mountain Ranges Of Mongolia
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 and ...
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Mountain Ranges Of Russia
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 and ...
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Ubsunur Hollow Biosphere Reserve
Uvs Lake Basin (also Uvs Nuur Basin or Ubs Nuur Basin; mn, Увс нуурын хотгор, Uws nuuriin hotgor) is an endorheic basin located on the territorial border of Mongolia and Tuva, a republic of the Russian Federation. The basin is part of the Central Asian Internal Drainage Basin and is named after Uvs Lake (Uvs Nuur, Ubsu Nur), a large saline lake situated in the western part of its drainage basin and is one of the last remnants of the mammoth steppes. Uvs Lake is a shallow lake with an area of . Its entire basin, which includes several smaller lakes, is . Uvs Lake Basin may also refer to Ubsunur Hollow (Russian: Убсунурская котловина, ''Ubsunorskaya Kotlovina''), which is the western part of the drainage basin, or to over of protected areas covering the lake and its surroundings. The hollow forms the northern part of the Great Lakes Depression, which has a surface of over . The hollow, and most of the drainage basin, are situated in the Khövsgö ...
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Uvs Nuur Basin
Uvs Lake Basin (also Uvs Nuur Basin or Ubs Nuur Basin; mn, Увс нуурын хотгор, Uws nuuriin hotgor) is an endorheic basin located on the territorial border of Mongolia and Tuva, a republic of the Russian Federation. The basin is part of the Central Asian Internal Drainage Basin and is named after Uvs Lake (Uvs Nuur, Ubsu Nur), a large saline lake situated in the western part of its drainage basin and is one of the last remnants of the mammoth steppes. Uvs Lake is a shallow lake with an area of . Its entire basin, which includes several smaller lakes, is . Uvs Lake Basin may also refer to Ubsunur Hollow (Russian: Убсунурская котловина, ''Ubsunorskaya Kotlovina''), which is the western part of the drainage basin, or to over of protected areas covering the lake and its surroundings. The hollow forms the northern part of the Great Lakes Depression, which has a surface of over . The hollow, and most of the drainage basin, are situated in the Khövsgö ...
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Tuva Depression
Tuva Depression ( rus, Тувинская котловина, r=Tuvinskaya kotlovina) is located among mountains of South Central Siberia — the Tannu-Ola Mountains, Eastern Sayans and Western Sayans, and the Altay Mountains region. It is part of a region with a combination of raised lands and depressions. This Tuva Depression is within the Tuva Republic. The elevation of the depression varies between . See also *Depression (geology) *Kuznetsk Depression *Minusinsk Depression *Geography of South-Central Siberia South Central Siberia is a geographical region north of the point where Russia, China, Kazakhstan and Mongolia come together. Regions of Asia North Asia The Four Corners At approximately , the borders of Russia, China, Mongolia and Kaza ... References External links Central Siberia Depressions of Russia Landforms of Tuva Geology of Siberia Geography of Central Asia {{Tuva-geo-stub ...
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Great Soviet Encyclopedia
The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya entsiklopediya'' (or '' Great Russian Encyclopedia'') in an updated and revised form. The GSE claimed to be "the first Marxist–Leninist general-purpose encyclopedia". Origins The idea of the ''Great Soviet Encyclopedia'' emerged in 1923 on the initiative of Otto Schmidt, a member of the Russian Academy of Sciences. In early 1924 Schmidt worked with a group which included Mikhail Pokrovsky, (rector of the Institute of Red Professors), Nikolai Meshcheryakov (Former head of the Glavit, the State Administration of Publishing Affairs), Valery Bryusov (poet), Veniamin Kagan (mathematician) and Konstantin Kuzminsky to draw up a proposal which was agreed to in April 1924. Also involved was Anatoly Lunacharsky, People's Commissar of Education ...
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Altai Republic
The Altai Republic (; russian: Респу́блика Алта́й, Respublika Altay, ; Altai: , ''Altay Respublika''), also known as Gorno-Altai Republic, and colloquially, and primarily referred to in Russian to distinguish from the neighbouring Altai Krai as the Gornyi Altai (russian: Горный Алтай, lit=the mountainous Altai), is a republic of Russia located in southern Siberia. It is a part of the Siberian Federal District, and covers an area of ; with a population of 210,924 residents. It is the least-populous republic of Russia and least-populous federal subject in the Siberian Federal District. Gorno-Altaysk is the capital and the largest town of the republic. The Altai Republic is one of Russia's ethnic republics, primarily representing the indigenous Altai people, a Turkic ethnic group that form 35% of the Republic's population, while ethnic Russians form a majority at 57%, and with minority populations of Kazakhs, other Central Asian ethnicities, and Germa ...
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Uvs Nuur
Uvs Lake ( mn, Увс нуур, Uws nuur, ; russian: Озеро Убсу-Нур, Ozero Ubsu-Nur; zh, 乌布苏湖, wū bù sū hú, pinyin: ''Wū Bù Sū hú'') is a highly saline lake in an endorheic basin—Uvs Nuur Basin in Mongolia with a small part in Russia. It is the largest lake in Mongolia by surface area, covering 3,350 km2 at 759 m above sea level. The northeastern tip of the lake is situated in the Tuva Republic of the Russian Federation. The largest settlement near the lake is Ulaangom. This shallow and very saline body of water is a remainder of a huge saline sea which covered a much larger area several thousand years ago. Name The name Uvs Nuur (sometimes spelled Ubsa Nor or Ubsunur) derives from ''subsen'', a Turkic/Mongolian word referring to the bitter dregs left behind in the making of airag (Mongolian milk wine), and ''nuur'', the Mongolian word for lake. The name is a reference to the lake's salty, undrinkable water. In one Mongolian folk tale ...
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Altay Mountains
The Altai Mountains (), also spelled Altay Mountains, are a mountain range in Central Asia, Central and East Asia, where Russia, China, Mongolia and Kazakhstan converge, and where the rivers Irtysh and Ob River, Ob have their headwaters. The massif merges with the Sayan Mountains in the northeast, and gradually becomes lower in the southeast, where it merges into the high plateau of the Gobi Desert. It spans from about 45° to 52° N and from about 84° to 99° E. The region is inhabited by a sparse but ethnically diverse population, including Russian people, Russians, Kazakh people, Kazakhs, Altai people, Altais, Mongol people, Mongols and Volga Germans, though predominantly represented by indigenous ethnic minorities of semi-nomadic stock. The local economy is based on bovine, sheep, horse animal husbandry, husbandry, hunting, agriculture, forestry, and mining. The Altaic languages, Altaic language family takes its name from this mountain range. Etymology and modern names ...
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Steppes
In physical geography, a steppe () is an ecoregion characterized by grassland plains without trees apart from those near rivers and lakes. Steppe biomes may include: * the montane grasslands and shrublands biome * the temperate grasslands, savannas and shrublands biome A steppe may be semi-arid or covered with grass or with shrubs or with both, depending on the season and latitude. The term " steppe climate" denotes the climate encountered in regions too dry to support a forest but not dry enough to be a desert. Steppe soils are typically of the chernozem type. Steppes are usually characterized by a semi-arid or continental climate. Extremes can be recorded in the summer of up to and in winter, . Besides this major seasonal difference, fluctuations between day and night are also very great. In both the highlands of Mongolia and northern Nevada, can be reached during the day with sub-freezing readings at night. Mid-latitude steppes feature hot summers and cold winte ...
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