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The Karakoram (, ) is a in Asia located primarily in the region. The range spans the borders of , , and , with the north-western extremities of the range extending into and . The Karakoram contains four of the fourteen , the highest of which is K2, the second highest mountain on Earth.

The Karakoram begins in the in western Afghanistan and extends eastwards into Indian-administered and Chinese-administered , as well as the Chinese province of . Most of the Karakoram is located within the Pakistani-administered region. The Karakoram is bounded on the east by the plateau, on the north-east by the edge of the , and on the north by the river valleys of the and , beyond which lie the . At the north-west corner are the . The southern boundary of the Karakoram is formed west to east by the , , and , which separate the range from the north-western end of the . These rivers flow north-west before making an abrupt turn south-westwards towards the plains of . Roughly in the middle of the Karakoram range is the , which was part of a now unused trade route between and .

The range is about in length and is the most place on Earth outside the polar regions. The ( long) and ( long) are the second- and third-longest glaciers outside the polar regions.Tajikistan's Fedchenko Glacier is long. Baltoro and Batura Glaciers in the Karakoram are long, as is Bruggen or Pio XI Glacier in southern Chile. Measurements are from recent imagery, generally supplemented with Russian 1:200,000 scale topographic mapping as well as Jerzy Wala, Orographical Sketch Map: Karakoram: Sheets 1 & 2, , , 1990. The Karakoram is the on Earth and part of a complex of ranges that includes the , , and the .. The range contains eighteen summits higher than in , with four above . which include K2, , , and .


Name
Karakoram is a term meaning black gravel. The Central Asian traders originally applied the name to the .
(2026). 9788120617940, Asian Educational Services. .
Early European travelers, including William Moorcroft and George Hayward, started using the term for the range of mountains west of the pass, although they also used the term Muztagh (meaning, "Ice Mountain") for the range now known as Karakoram. Later terminology was influenced by Thomas Montgomerie of the Survey of India, who gave the labels K1 to K6 (K for Karakoram) to six high mountains visible from his station at in the 1850s. These codes were extended up to more than thirty.

In traditional Indian geography, the mountains were known as Krishnagiri (black mountains), Kanhagiri, and Kanheri.


Exploration
Due to its altitude and ruggedness, the Karakoram is much less inhabited than parts of the further east. European explorers first visited in the early 19th century, followed by British surveyors starting in 1856.

The was crossed in 1887 by the expedition of Colonel Francis Younghusband,. (1994). Younghusband: The Last Great Imperial Adventurer, pp. 53, 56-60. HarperCollins Publishers, London. Reprint (1995): Flamingo. London. . and the valleys above the were explored by General Sir George K. Cockerill in 1892. Explorations in the 1910s and 1920s established most of the geography of the region.

The name Karakoram was used in the early 20th century, for example by Kenneth Mason, for the range now known as the . The term is now used to refer to the entire range from the above in the west to the in the bend of the in the east.

Floral surveys were carried out in the Shyok River catchment and from Panamik to Turtuk village by Chandra Prakash Kala during 1999 and 2000.


Geology and glaciers
The Karakoram is in one of the world's most geologically active areas, at the plate boundary between the Indo-Australian plate and the Eurasian plate. A significant part, somewhere between 28 and 50 percent, of the Karakoram Range is glaciated, covering an area of more than , compared to between 8 and 12 percent of the Himalaya and 2.2 percent of the . Mountain may serve as an indicator of climate change, advancing and receding with long-term changes in temperature and precipitation. The Karakoram glaciers are slightly retreating, unlike the Himalayas, where glaciers are losing mass at a significantly higher rate, many Karakoram glaciers are covered in a layer of rubble which insulates the ice from the warmth of the sun. Where there is no such insulation, the rate of retreat is high.


Ice Age
In the last , a stretched from western to , and from the to the . (glacier maps downloadable) To the south, the was the main valley glacier, which flowed down from the massif to elevation. In the north, the Karakoram glaciers joined those from the and flowed down to in the Tarim Basin.

While the current valley glaciers in the Karakoram reach a maximum length of , several of the ice-age valley glacier branches and main valley glaciers, had lengths up to . During the Ice Age, the glacier snowline was about lower than today.


Highest peaks
The majority of the highest peaks are in the Gilgit–Baltistan region administered by Pakistan. Baltistan has more than 100 mountain peaks exceeding height from sea level. Following is a list for the highest peaks of the Karakoram. Included are some of the mountains named with a K code, the most well-known of which is the K2.

K2 2K2, at the head of the Godwin-Austen Glacier
11K5
12
13K4
K3a
17K3
19
21
22K1
25
26
28
I 31K10
II K11
I 35K22
36
38
Sar 39
43
47K35
II 48
III 51
53
54
Yukshin Gardan Sar 55
I 56
58
K12 or 61K12 subsidiary of
63
Skilma Gangri or Ghursay Kangri II K8, on the western flank of the
64
66
67
69
70
71
74
Bojohagur Duanasir
Yazghil Dome South
81
Crown Peak 83
86
87
88K6
90
92
I 95
97
Gamba Gangri(approx) K9 near
Gomgma Gangri K7 at the head of the
K13 south west of
K25 south of


Subranges
The naming and division of the various subranges of the Karakoram is not universally agreed upon. However, the following is a list of the most important subranges, following Jerzy Wala.Jerzy Wala, Orographical Sketch Map of the Karakoram, Swiss Foundation for Alpine Research, Zurich, 1990. The ranges are listed roughly west to east.


Passes
Passes from west to east are:

The Khunjerab Pass is the only motorable pass across the range. The Shimshal Pass (which does not cross an international border) is the only other pass still in regular use.


Cultural references
The Karakoram mountain range has been referred to in a number of and movies. refers to the Karakoram mountain range in his novel Kim, which was first published in 1900. made a film titled Karakoram, chronicling a French expedition to the range in 1936. The film won the Silver Lion at the Venice Film Festival of 1937. details the Karakoram, and specifically K2 and the , extensively in his book Three Cups of Tea, about his quest to build schools for children in the region. K2 Kahani (The K2 Story) by Mustansar Hussain Tarar describes his experiences at K2 base camp.
(1994). 9789693505238, Sang-e-Meel (published in Urdu).


See also
  • Karakoram Highway
  • List of mountain ranges of the world
  • List of highest mountains (a list of mountains above )


Citations

Sources
  • Curzon, George Nathaniel. 1896. The Pamirs and the Source of the Oxus. Royal Geographical Society, London. Reprint: Elibron Classics Series, Adamant Media Corporation. 2005. (pbk); (hbk).
  • 2002. Kim (novel); ed. by Zohreh T. Sullivan. New York: W. W. Norton & Company. —This is the most extensive critical modern edition with footnotes, essays, maps, etc.
  • and Relin, David Oliver. 2008. Three Cups of Tea. Penguin Books Ltd. (pbk); Viking Books (hbk); Tantor Media (MP3 CD).
  • Kreutzmann, Hermann, Karakoram in Transition: Culture, Development, and Ecology in the Hunza Valley, Oxford, Oxford University Press, 2006. .


Further reading


External links

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