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Kunlun Mountains
The Kunlun Mountains constitute one of the longest mountain chains in Asia, extending for more than 3,000 kilometres (1,900 mi). In the broadest sense, the chain forms the northern edge of the Tibetan Plateau south of the Tarim Basin. Located in Western China, the Kunlun Mountains have been known as the "Forefather of Mountains" in China.
The exact definition of the Kunlun Mountains varies over time. Older sources used Kunlun to mean the mountain belt that runs across the center of China, that is, Altyn Tagh along with the Qilian and Qin Mountains. Recent sources have the Kunlun range forming most of the south side of the Tarim Basin and then continuing east, south of the Altyn Tagh. Sima Qian (Records of the Grand Historian, scroll 123) says that Emperor Wu of Han sent men to find the source of the Yellow River and gave the name Kunlun to the mountains at its source. The name seems to have originated as a semi-mythical location in the classical Chinese text Classic of Mountains and Seas.
From the Pamirs of Tajikistan, the Kunlun Mountains run east through southern Xinjiang to Qinghai province. They stretch along the southern edge of what is now called the Tarim Basin, the infamous Taklamakan desert, and the Gobi Desert. A number of important rivers flow from the range including the Karakash River ('Black Jade River') and the Yurungkash River ('White Jade River'), which flow through the Khotan Oasis into the Taklamakan Desert. To the south of the Kunlun is the sparsely populated Changtang region, which forms part of the Tibetan Plateau.
Altyn-Tagh or Altun Range is one of the chief northern ranges of the Kunlun. Its northeastern extension Qilian Shan is another main northern range of the Kunlun. In the south main extension is the Min Shan. Bayan Har Mountains, a southern branch of the Kunlun Mountains, forms the watershed between the catchment basins of China's two longest rivers, the Yangtze River and the Yellow River.
The highest mountain of the Kunlun Mountains is the Kunlun Goddess Peak (7,167 m) in the Keriya area of the western Kunlun Mountains.
Some authorities[who?] claim that the Kunlun extends further northwest-wards as far as Kongur Tagh (7,649 m) and the famous Muztagh Ata (7,546 m).[citation needed]
But these mountains are physically much more closely linked to the Pamir group (ancient Mount Imeon). The Arka Tagh (Arch Mountain) is in the center of the Kunlun Mountains; its highest points are Ulugh Muztagh (6,973 m) and Bukadaban Feng (6,860 m). In the eastern Kunlun Mountains the highest peaks are Yuzhu Peak (6,224 m) and Amne Machin [also Dradullungshong] (6,282 m); the latter is the major eastern peak of the Kunlun Mountains and is thus considered as the eastern edge of the Kunlun Mountains.
The mountain range formed at the northern edges of the Cimmerian Plate during its collision, in the Late Triassic, with Siberia, which resulted in the closing of the Paleo-Tethys Ocean.
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Kunlun Mountains
The Kunlun Mountains constitute one of the longest mountain chains in Asia, extending for more than 3,000 kilometres (1,900 mi). In the broadest sense, the chain forms the northern edge of the Tibetan Plateau south of the Tarim Basin. Located in Western China, the Kunlun Mountains have been known as the "Forefather of Mountains" in China.
The exact definition of the Kunlun Mountains varies over time. Older sources used Kunlun to mean the mountain belt that runs across the center of China, that is, Altyn Tagh along with the Qilian and Qin Mountains. Recent sources have the Kunlun range forming most of the south side of the Tarim Basin and then continuing east, south of the Altyn Tagh. Sima Qian (Records of the Grand Historian, scroll 123) says that Emperor Wu of Han sent men to find the source of the Yellow River and gave the name Kunlun to the mountains at its source. The name seems to have originated as a semi-mythical location in the classical Chinese text Classic of Mountains and Seas.
From the Pamirs of Tajikistan, the Kunlun Mountains run east through southern Xinjiang to Qinghai province. They stretch along the southern edge of what is now called the Tarim Basin, the infamous Taklamakan desert, and the Gobi Desert. A number of important rivers flow from the range including the Karakash River ('Black Jade River') and the Yurungkash River ('White Jade River'), which flow through the Khotan Oasis into the Taklamakan Desert. To the south of the Kunlun is the sparsely populated Changtang region, which forms part of the Tibetan Plateau.
Altyn-Tagh or Altun Range is one of the chief northern ranges of the Kunlun. Its northeastern extension Qilian Shan is another main northern range of the Kunlun. In the south main extension is the Min Shan. Bayan Har Mountains, a southern branch of the Kunlun Mountains, forms the watershed between the catchment basins of China's two longest rivers, the Yangtze River and the Yellow River.
The highest mountain of the Kunlun Mountains is the Kunlun Goddess Peak (7,167 m) in the Keriya area of the western Kunlun Mountains.
Some authorities[who?] claim that the Kunlun extends further northwest-wards as far as Kongur Tagh (7,649 m) and the famous Muztagh Ata (7,546 m).[citation needed]
But these mountains are physically much more closely linked to the Pamir group (ancient Mount Imeon). The Arka Tagh (Arch Mountain) is in the center of the Kunlun Mountains; its highest points are Ulugh Muztagh (6,973 m) and Bukadaban Feng (6,860 m). In the eastern Kunlun Mountains the highest peaks are Yuzhu Peak (6,224 m) and Amne Machin [also Dradullungshong] (6,282 m); the latter is the major eastern peak of the Kunlun Mountains and is thus considered as the eastern edge of the Kunlun Mountains.
The mountain range formed at the northern edges of the Cimmerian Plate during its collision, in the Late Triassic, with Siberia, which resulted in the closing of the Paleo-Tethys Ocean.