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Mongolia's largest lake by area, Uvs Lake is in the Great Lakes Depression. Mongolia's largest lake by volume of water, Lake Khövsgöl, drains via the Selenge river to the Arctic Ocean. One of the most easterly lakes of Mongolia, Hoh Nuur, at an elevation of 557 metres, is the lowest point in the country. [7]
The Gobi Desert (Mongolian: Говь, ᠭᠣᠪᠢ, / ˈ ɡ oʊ b i /; Chinese: 戈壁; pinyin: gēbì) is a large, cold desert and grassland region located in northern China and southern Mongolia. It is the sixth largest desert in the world .
An enlargeable map of Mongolia. The following outline is provided as an overview of and topical guide to Mongolia: Mongolia is a landlocked sovereign state in East Asia. It borders Russia to the north and China to the south. Ulaanbaatar, the capital and largest city, is home to about 38% of the population.
Gobi Desert (45 P) Pages in category "Deserts of Mongolia" The following 4 pages are in this category, out of 4 total. This list may not reflect recent changes. D.
Khongoryn Els sand dunes. Mongolia has three types of deserts, and some of it has enough grass for livestock to graze, but the Khongoryn Els, in the extreme south of the Gobi Desert, has a huge range of sand dunes – 6–12 kilometres (3.7–7.5 mi) wide, 100 kilometres (62 mi) long (180 kilometres (110 mi) is also mentioned [5]) [6] and rising to a height of 80 metres (260 ft) (a maximum ...
The reserve was established in 1975 and declared an International Biosphere Reserve in 1991. It comprises about 9000 km 2 of desert steppe, arid mountains, deserts and semi deserts. Temperatures can fall to -40 °C in winter and rise to +40 °C in the summer.
Alashan Plateau semi-desert (Mongolia, China) Eastern Gobi desert steppe (Mongolia, China) Gobi Lakes Valley desert steppe (Mongolia, China) Great Lakes Basin desert steppe (Mongolia, Russia) Junggar Basin semi-desert (China, Mongolia, Kazakhstan
Mongolia has complicated tectonic and structural geology, belonging to the Mongolian-Okhotsk Mobile Zone, between the Siberian Platform and Chinese Platform.The basement rocks formed during the Paleozoic in the Precambrian as Riphean age ophiolite formations experienced rifting from 1.7 to 1.6 billion years ago and again around 800 million years ago.