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Yamdrok Lake. 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 a plateau region in Asia and the home to the indigenous Tibetan people. With an average elevation of 4,900 metres (16,000 ft), it is the highest region on Earth and is commonly referred to as the "Roof of the World." A unified Tibet first came into being under Songtsen Gampo in the 7th century.
The United Nations geoscheme is a system which divides 248 countries and territories in the world into six continental regions, 22 geographical subregions, and two intermediary regions. [1] It was devised by the United Nations Statistics Division (UNSD) based on the M49 coding classification . [ 2 ]
The Tibetan name for their land, Bod (བོད་), means 'Tibet' or 'Tibetan Plateau', although it originally meant the central region around Lhasa, now known in Tibetan as Ü (དབུས). [ citation needed ] The Standard Tibetan pronunciation of Bod ( [pʰøʔ˨˧˨] ) is transcribed as: Bhö in Tournadre Phonetic Transcription ; Bö in ...
Amdo is one of the traditional regions of Greater or ethnographic Tibet. [1] The other regions are Ü-Tsang, also known as political or central Tibet, to the west and Kham to the southeast. [3] Historically, Amdo and Kham together were also called Do Kham on maps and manuscripts. [4]
A world map is a map of most or all of the surface of Earth. World maps, because of their scale, must deal with the problem of projection. Maps rendered in two dimensions by necessity distort the display of the three-dimensional surface of the Earth. While this is true of any map, these distortions reach extremes in a world map.
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