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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 .
The Tibetan Plateau, [a] also known as Qinghai–Tibet Plateau [b] and Qing–Zang Plateau, [c] is a vast elevated plateau located at the intersection of Central, South, and East Asia. [ d ] Geographically, it is located to the north of Himalayas and the Indian subcontinent , and to the south of Tarim Basin and Mongolian Plateau .
Tibet is the highest region on Earth, with an average elevation of 4,380 m (14,000 ft). [4] [5] Located in the Himalayas, the highest elevation in Tibet is Mount Everest, Earth's highest mountain, rising 8,848 m (29,000 ft) above sea level. [6] The Tibetan Empire emerged in the 7th century.
For the Bon people, the mountain is the abode of sky goddess Sipaimen and the mountain was the centre of the ancient Bon empire of Zhang Zhung. [12] [81] [82] As per Tibetan beliefs, the mountain was the centre of the universe Mandala and the source of the mythical Lion, Horse, Peacock, and Elephant Rivers which flowed in the four cardinal ...
The mountains are known as the Himālaya in Nepali and Hindi (both written हिमालय), Hinvāl (हिंवाळ) in Garhwali, Himāl (हिमाल) in Kumaoni, the Himalaya (ཧི་མ་ལ་ཡ་) or 'The Land of Snow' (གངས་ཅན་ལྗོངས་) in Tibetan, also known as Himālaya in Sinhala (written as ...
Pages in category "Mountains of Tibet" The following 66 pages are in this category, out of 66 total. This list may not reflect recent changes. B. Bairiga; C. Changla;
Dakpa Sheri [c] (Tibetan: དག་པ་ཤེལ་རི, Wylie: dag pa shel ri, THL: dak pa shel ri, [7] Chinese: 达瓜西热; pinyin: Dá guā xī rè), explained as "Pure Crystal Mountain" and also known as Tsari (Tibetan: རྩ་རི, Wylie: rtsa ri), is a mountain in the eponymously named Tsari region in Lhöntse County of Tibet's Shannan Prefecture.
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