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The Tibetan Plateau (), also known in China as the Qinghai–Tibet Plateau or the Qingzang Plateau () or Himalayan Plateau, is a vast elevated plateau in Central Asia〔''Illustrated Atlas of the World'' (1986) Rand McNally & Company. ISBN 0-528-83190-9 pp. 164-5〕〔''Atlas of World History'' (1998 ) HarperCollins. ISBN 0-7230-1025-0 pg. 39〕〔(【引用サイトリンク】The Tibetan Empire in Central Asia (Christopher Beckwith) )〕〔Hopkirk 1983, pg. 1〕 and East Asia, covering most of the Tibet Autonomous Region and Qinghai Province in western China, as well as part of Ladakh in Jammu and Kashmir state of India. It stretches approximately north to south and east to west. With an average elevation exceeding , the Tibetan Plateau is sometimes called "the Roof of the World" and is the world's highest and largest plateau, with an area of (about five times the size of Metropolitan France). Sometimes termed the "Third Pole", the Tibetan Plateau is the headwaters of the drainage basins of most of the streams in surrounding regions. Its tens of thousands of glaciers and other geographical and ecological features serve as a "water tower" storing water and maintaining flow. The impact of global warming on the Tibetan Plateau is of intense scientific interest. ==Description== The Tibetan Plateau is surrounded by massive mountain ranges.〔 〕 The plateau is bordered to the south by the Himalayan range, to the north by the Kunlun Range which separates it from the Tarim Basin, and to the northeast by the Qilian Range which separates the plateau from the Hexi Corridor and Gobi Desert. To the east and southeast the plateau gives way to the forested gorge and ridge geography of the mountainous headwaters of the Salween, Mekong, and Yangtze rivers in western Sichuan (the Hengduan Mountains) and southwest Qinghai. In the west the curve of the rugged Karakoram range of northern Kashmir embraces it. The Tibetan Plateau is bounded on the north by a broad escarpment where the altitude drops from around to in less than . Along the escarpment is a range of mountains. In the west the Kunlun Mountains separate the plateau from the Tarim Basin. About half way across the Tarim the bounding range becomes the Altyn-Tagh and the Kunluns, by convention, continue somewhat to the south. In the 'V' formed by this split is the western part of the Qaidam Basin. The Altyn-Tagh ends near the Dangjin pass on the Dunhuang-Golmud road. To the west are short ranges called the Danghe, Yema, Shule and Tulai Nanshans. The easternmost range is the Qilian Mountains. The line of mountains continues east of the plateau as the Qin Mountains which separate the Ordos Region from Sichuan. North of the mountains runs the Gansu or Hexi Corridor which was the main silk-road route from China proper to the west. The plateau is a high-altitude arid steppe interspersed with mountain ranges and large brackish lakes. Annual precipitation ranges from and falls mainly as hailstorms. The southern and eastern edges of the steppe have grasslands which can sustainably support populations of nomadic herdsmen, although frost occurs for six months of the year. Permafrost occurs over extensive parts of the plateau. Proceeding to the north and northwest, the plateau becomes progressively higher, colder and drier, until reaching the remote Changthang region in the northwestern part of the plateau. Here the average altitude exceeds and winter temperatures can drop to . As a result of this extremely inhospitable environment, the Changthang region (together with the adjoining Kekexili region) is the least populous region in Asia, and the third least populous area in the world after Antarctica and northern Greenland. Image:TibetplateauA2002144.0440.500m.jpg|NASA satellite image of the south-eastern area of Tibetan Plateau. Brahmaputra River is in the lower right. Image:Himalaya composite.jpg|The Tibetan Plateau lies between the Himalayan range to the south and the Taklamakan Desert to the north. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Tibetan Plateau」の詳細全文を読む スポンサード リンク
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