Pamir Mountains

Located in Central Asia, the Pamir Mountains are formed by the junction of the Tian Shan, Karakoram, Kunlun, and Hindu Kush ranges. They are among the world's highest mountains. They are also known by the Chinese name of Congling.

The Pamir region is centered in the Tajikistani region of Gorno-Badakhshan. Parts of the Pamir also lie in the countries of Kyrgyzstan, Afghanistan, and Pakistan. South of Gorno-Badakhshan, the Wakhan Corridor runs through the Pamir region, which also includes the northern extremes of the North-West Frontier Province and the northern extremes of the Northern Areas of Pakistan.

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Geography

Its two highest mountains are Ismail Samani Peak (from 19321962 known as Stalin Peak, from 19621998 as Communism Peak), 24,590 ft (7,495 m) and Lenin Peak, 23,508 ft (7,165 m).

There are many glaciers in the Pamir Mountains, including the 144 mi (231 km) long Fortambek glacier, the longest in the former USSR.

Climate

Covered in snow throughout the year, the Pamirs have long and bitterly cold winters, and short, cool summers. Annual precipitation is about 5 inches (130 mm), which supports grasslands but few trees.

Economy

Coal is mined in the west, though sheep herding in upper meadowlands are the primary source of income for the area.

Discoveries

In the early 1980s, a deposit of gemstone-quality clinohumite was discovered in the Pamir Mountains. It was the only such deposit known until the discovery of gem-quality material in the Taymyr region of Siberia in 2000.

Transportation

At the southeastern edge of the Pamir region, in China, the highest international highway in the world, the Karakoram Highway, connects Pakistan to China.

Further Reading

See also


There was also a sailing ship named Pamir.

See also: Pamir Mountains, 1932, 1962, 1980s, 1998, 2000, Afghanistan, Central Asia, China, Clinohumite