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Southern Tibet [1] [2] [3] is a literal translation of the Chinese term "藏南" (pinyin: Zàng Nán), which may refer to different geographic areas: . The southern part of Tibet, covering the middle reaches of the Yarlung Tsangpo River Valley between Saga County to the west and Mainling County to the east, as well as neighbouring areas located between the Himalayas to the south and the ...
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.
The main problem that the South Tibetan detachment is expected to help resolve is the method of emplacement of the GHC between the LHS and THS within the Himalaya. [5] There are three models that help explain this emplacement: wedge extrusion, channel flow , and tectonic wedging .
Of the resident population of the Tibet Autonomous Region, 3,204,700 were Tibetans and other ethnic minorities, of whom 3,137,900 were Tibetans, an increase of 421,500, or 15.52%, over 2010, with an average annual growth rate of 1.45%; 66,800 were other ethnic minorities, an increase of 26,300, or 64.95%, over 2010, with an average annual ...
It is located in the southern part of the Tibet Autonomous Region and the south-central part of Xigazê. [6] It borders Dinggyê County and Sa'gya County to the east, Nyalam County to the west, Ngamring County to the north, Lhatse County to the northeast, and Nepal to the south. [6]
The current borders of the Tibet Autonomous Region were generally established in the 18th century [8] and include about half of historical Tibet. The Tibet Autonomous Region spans over 1,200,000 km 2 (460,000 sq mi), and is the second-largest province-level division of China by area, after Xinjiang. Due to its harsh and rugged terrain, it is ...
Seven north–south trending rifts and normal faults were first discovered in southern Tibet during the late 1970s and early 1980s using satellite imagery. They began formation when extension occurred some 4 to 8 million years ago. [21] The largest earthquakes in Tibet, with magnitudes of 8.0 or similar, occur along strike-slip faults.
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 .