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・ Geological Survey of Denmark and Greenland
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Geography of Tibet
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Geography of Tibet : ウィキペディア英語版
Geography of Tibet

The geography of Tibet consists of the high mountains, lakes and rivers lying between Central, East and South Asia. Traditionally, Western (European and American) sources have regarded Tibet as being in Central Asia, though today's maps show a trend toward considering all of modern China, including Tibet, to be part of East Asia.〔(【引用サイトリンク】title=UNESCO Collection of History of Civilizations of Central Asia Volume IV )Tibet is often called "the roof of the world," comprising table-lands averaging over 4,950 metres above the sea with peaks at 6,000 to 7,500 m, including Mount Everest, on the border with Nepal.
==Description==
It is bounded on the north and east by the Central China Plain, on the west by the Kashmir Region of India and on the south by Nepal, India and Bhutan. Most of Tibet sits atop a geological structure known as the Tibetan Plateau, which includes the Himalaya and many of the highest mountain peaks in the world.
High mountain peaks include Changtse, Lhotse, Makalu, Gauri Sankar, Gurla Mandhata, Cho Oyu, Jomolhari, Gyachung Kang, Gyala Peri, Mount Kailash, Kawagebo, Khumbutse, Melungtse, Mount Nyainqentanglha, Namcha Barwa, Shishapangma and Yangra.
Mountain passes include Cherko la and North Col. Smaller mountains include Mount Gephel and Gurla Mandhata.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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