Central Asian Internal Drainage Basin
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Central Asian Internal Drainage Basin
The Central Asian Internal Drainage Basin or Central Asian Inland Basin is the largest of 3 major hydrological basins that cover Mongolia (cf. Arctic Drainage Basin & Pacific Drainage Basin). It is an endorheic basin.Ayurin Dulmaa,Mongolian Limnology and Ichthyology in: "Mongolia Today: Science, Culture, Environment and Development" (2002) (quote from Google cache) The basin also includes much of the Western and Central Asia: the watersheds of the Great Lakes Depression, the Valley of Lakes, and the lowlands of the Gobi Desert. It is separated from the other two basins by the ridges of the Khangai Mountains and Khentii Mountains. The Khentii Mountains also separate Arcic and Pacific basins within Mongolia. It is further subdivided into local drainage basins. See also *List of drainage basins by area The list of drainage basins by area identifies basins (also known as "catchments" or, in North American usage, "watersheds"), sorted by area, which drain to oceans, mediterranea ...
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Continental Basins Of Mongolia - Asian Development Bank 2020
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Great Lakes Depression
The Great Lakes Depression ( mn, Их нууруудын хотгор, ''Ikh Nuuruudyn Khotgor''), also called the Great Lakes' Hollow, is a large semi-arid depression in Mongolia that covers parts of the Uvs, Khovd, Bayan-Ölgii, Zavkhan and Govi-Altai ''aimags''. Bounded by the Altai in the West, Khangai in the East and Tannu-Ola Mountains in the North, it covers the area of over with elevations from . Small northern parts of the depression are part of Russia."Great Lakes Depression"
''''
The depression is named so because it contains six major Mongolian lakes: saline

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Landforms Of Mongolia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ...
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Bodies Of Water Of Mongolia
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List Of Drainage Basins By Area
The list of drainage basins by area identifies basins (also known as "catchments" or, in North American usage, "watersheds"), sorted by area, which drain to oceans, mediterranean seas, rivers, lakes and other water bodies. All basins larger than are included as well as selected smaller basins. It includes drainage basins which do not flow to the ocean (endorheic basins). It includes oceanic sea drainage basins which have hydrologically coherent areas (oceanic seas are set by IHO convention). The oceans drain approximately 83% of the land in the world. The other 17% – an area larger than the basin of the Arctic Ocean – drains to internal endorheic basins. There are also substantial areas of the world that do not "drain" in the commonly understood sense. In polar deserts, much of the snowfall sublimates directly into the air and does not melt into flowing water, while in tropical deserts precipitation may evaporate before joining any substantial water course. These areas can st ...
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Khentii Mountains
The Khentii Mountains ( mn, Хэнтийн нуруу) are a mountain range in the Töv and Khentii Provinces in North Eastern Mongolia. Geography The mountain chain overlaps the Khan Khentii Strictly Protected Area and includes Mongolia's sacred mountain, Burkhan Khaldun, which is associated with the origin of Genghis Khan. The range forms the watershed between the Arctic Ocean (via Lake Baikal) and the Pacific Ocean basins. Rivers originating in the range include the Onon, Kherlen, Menza and Tuul. A northern extension of the Khentii Mountains forms a range of the same name which is part of the Khentei-Daur Highlands in the Transbaikalia Krai of Russia. History The legendary Mongol Genghis Khan is thought to have chosen a resting place in the Khentii Mountains, called the Great Taboo, or Ikh Khorig The Ikh Khorig, or Great Taboo, is a area in the Khentii Aimag (province) of Mongolia, believed by some to be the location of Genghis Khan's grave. It has been carefully gua ...
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Khangai Mountains
The Khangai Mountains ( mn, Хангайн нуруу, Hangain nuruu, ); form a mountain range, range in central Mongolia, some west of Ulaanbaatar. Name Two provinces of Mongolia are named after the Khangai mountains: Arkhangai (North Khangai) and Ovorkhangai (South Khangai). The mild climate area where the two provinces meet (in eastern Khangai) is known as the cradle of Mongolian and nomadic civilization. The plains at the foot of the eastern Khangai host the Orkhon Valley, Orkhon Valley World Heritage Site. The Xiongnu capital Luut Khot (Lungcheng), the Xianbei state, Xianbei capital Ordo and the Rouran capital Moomt (Mume) are said to have been located there. Later empires also established their capitals there: e.g. the Uyghur Khaganate (745–840) built their capital Ordu-Baliq in the region. Features The tallest mountain is Otgontenger ( "Youngest sky"), which is about 4,000 metres tall. It is revered by the Mongols and state ceremonies are held there. Suvraga Khairkha ...
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Gobi Desert
The Gobi Desert (Chinese: 戈壁 (沙漠), Mongolian: Говь (ᠭᠣᠪᠢ)) () is a large desert or brushland region in East Asia, and is the sixth largest desert in the world. Geography The Gobi measures from southwest to northeast and from north to south. The desert is widest in the west, along the line joining the Lake Bosten and the Lop Nor (87°–89° east). In 2007, it occupied an arc of land in area. In its broadest definition, the Gobi includes the long stretch of desert extending from the foot of the Pamirs (77° east) to the Greater Khingan Mountains, 116–118° east, on the border of Manchuria; and from the foothills of the Altay, Sayan, and Yablonoi mountain ranges on the north to the Kunlun, Altyn-Tagh, and Qilian mountain ranges, which form the northern edges of the Tibetan Plateau, on the south. A relatively large area on the east side of the Greater Khingan range, between the upper waters of the Songhua (Sungari) and the upper waters of the Liao-h ...
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Valley Of Lakes
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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