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Geladaindong Peak

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Geladaindong Peak (also spelledGeladandong,Geladaintong orKolha Dardong) is a snow-covered mountain (ormassif) located in SouthwesternQinghai Province ofChina near the border ofTibet Autonomous Region.[2] It is the tallest mountain in theTanggula Mountain Range of theTibetan Plateau with an elevation of 6,621 metres (21,722 ft) abovesea level. The traditional source of theYangtze River, begins withglaciers on its surface. The Yangtze's true source, however, lies 325 km (202 mi) away at the head of the Dam Qu.

Geladaindong
The glaciers of the Tanggula Mountains, the traditional source of the Yangtze River
Highest point
Elevation6,621 m (21,722 ft)[1]
Prominence1,541 m (5,056 ft)[1]
ListingUltra
Coordinates33°29′45″N91°10′03″E / 33.49583°N 91.16750°E /33.49583; 91.16750[1]
Geography
Geladaindong is located in Tibetan Plateau
Geladaindong
Geladaindong
Location on Tibetan Plateau
LocationQinghai,China
Parent rangeTanggula
Climbing
First ascent1985 by a Japanese team

The mountain's name isGeladaindong in theTibetan language. The name inChinese is (Pinyin: Gèlādāndōng) or (Pinyin: Gèlādāndōng Fēng, literally "Geladandong Peak").

Location

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Geladaindong is located in the administrative unit known asTanggula Town: anexclave ofHaixi Prefecture, in the middle section of Tanggula Shan (the Tanggula Mountain Range).

The Geladaindong Peak is encircled by over twenty high peaks exceeding 6,000 meters (19,685 ft) in height. It is approximately 50 km (31 mi) long from north to south and approximately 20 km (12 mi) wide from west to east, covering an area of approximately 670 square kilometres (260 sq mi) with ice and snow, covered by over 40glaciers. This area is directly across the border fromAmdo County,Nagqu Prefecture,Tibet Autonomous Region.

TheQinghai-Tibet Railway crosses the Tanggula Mountain Range around 100 km (62 mi) to the east of Geladaindong Peak.

Climate

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Due to the area's arid climate, its annual precipitation is only 200 mm (7.9 in). In the high-altitude area of over 5,000 meters (16,404 ft), however, there exists violent local air circulation and its yearly precipitation is several hundred mm more than that in the foothill area. Thus,snow andhailstones frequently fall, presenting conditions for the development of glaciers. The average temperature is −5 °C (23 °F), and the hottest months are from June to August with a temperature of over 20 °C (68 °F), while the coldest month is January, with a temperature of −18 °C (−0.4 °F). In the high-altitude area of over 5,000 m (16,404 ft), it remains cold all year round, the lowest temperature being less than −30 °C (−22 °F).

Wildlife

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The mountain serves as a shelter for more than twenty kinds of wild animals, including thewhite-lipped deer, Asiaticwild ass,snow leopard, and alpinesnowcock.

Climbing

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Geladaindong was first climbed by Japanese team in 1985 after three years of trying to obtain a permit.[3] They ascended the peak via the northwest ridge approaching from the northeast.

In 1997 an American team climbed a new route up the northeast face (55–60°).[3] The team consisted of William N. Rom M.D., Dan Luchtel PhD, and Mark Newcomb. Mark Newcomb also pioneered a face solo route on the same expedition.

Although a dangerous peak to climb, Geladaindong is popular among Chinesemountain climbers. In 1994, the Mountaineering Association ofPeking University (MAPKU) became the first Chinese climbing team to reach the summit of Geladaindong.

References

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External links

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