Explain the Relief features of Karakoram range?[4]
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Explain the Relief features of Karakoram range?[4]
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Answer:
Because of their great height, the Karakorams exhibit heavy glaciation, particularly on the southern, more humid slopes. Glaciers of the central, highest mountains include Hispar, Chogo Lungma, Braldu, Biafo, Baltoro with its famous Concordia junction, and Siachen (which is some 45 miles [70 km] long).
Explanation:
INTRODUCTION:
Karakoram Range, Chinese (Pinyin) Karakorum Shan or (Wade-Giles romanization) K’a-la-k’un-lun Shan, great mountain system extending some 300 miles (500 km) from the easternmost extension of Afghanistan in a southeasterly direction along the watershed between Central and South Asia. Found there are the greatest concentration of high mountains in the world and the longest glaciers outside the high latitudes. The Karakorams are part of a complex of mountain ranges at the centre of Asia, including the Hindu Kush to the west, the Pamirs to the northwest, the Kunlun Mountains to the northeast, and the Himalayas to the southeast. The borders of Tajikistan, China, Pakistan, Afghanistan, and India all converge within the Karakoram system, giving this remote region great geopolitical significance. The name “Kurra-koorrum,” a rendering of the Turkic term for “Black Rock” or “Black Mountain,” appeared in early 19th-century English writings.
MORE TO KNOW:
The Karakorams consist of a group of parallel ranges with several spurs. Only the central part is a monolithic range. The width of the system is about 150 miles (240 km); the length is increased from 300 miles (500 km) to 500 miles (800 km) if its easternmost extension—the Chang Chenmo (Chinese: Qiangchenmo) and Pangong ranges of the Plateau of Tibet—is included. The system occupies about 80,000 square miles (207,000 square km). The average elevation of mountains in the Karakorams is about 20,000 feet (6,100 metres), and four peaks exceed 26,000 feet (7,900 metres); the highest, K2 (Mount Godwin Austen), at 28,251 feet (8,611 metres), is the second highest peak in the world.
CHARACTERISTICS:
The topography is characterized by craggy peaks and steep slopes. The southern slopes are long and steep, the northern slopes steep and short. Cliffs and taluses (great accumulations of large fallen rocks) occupy a vast area. In the intermontane valleys, rocky inclines occur widely. Transverse valleys usually have the appearance of narrow, deep, steep ravines.
Explanation:
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