Karakoram Explained

Karakoram
Subdivision2 Type:Regions/Provinces
Country Type:Countries
Highest:K2
Elevation M:8611
Coordinates:35.8825°N 76.5133°W
Length Km:500
Range Coordinates:36°N 76°W
Karakoram
L:"Kara-Kunlun mountain range"
P:Kālǎ Kūnlún shānmài
Showflag:p
Uig:قاراقورام
Tib:ཁར་ཁོ་རུམ་རི
Wylie:kha ra kho rum ri

The Karakoram is a mountain range in the Kashmir region spanning the border of Pakistan, China, and India, with the northwestern extremity of the range extending to Afghanistan and Tajikistan. Most of the Karakoram mountain range falls under the jurisdiction of Gilgit-Baltistan, which is controlled by Pakistan. Its highest (and the world's second-highest) peak, K2, is located in Gilgit-Baltistan, Pakistan. It begins in the Wakhan Corridor (Afghanistan) in the west, encompasses the majority of Gilgit-Baltistan, Pakistan and extends into Ladakh (controlled by India) and Aksai Chin (controlled by China). It is part of the larger Trans-Himalayan mountain ranges.

The Karakoram is the second-highest mountain range on Earth and part of a complex of ranges that includes the Pamir Mountains, Hindu Kush, and Himalayas.[1] [2]

The range contains 18 summits higher than in elevation, with four above :[3] [4] [5] K2 (AMSL) (the second-highest peak on Earth), Gasherbrum I, Broad Peak, and Gasherbrum II.

The range is about in length and is the most glaciated place on Earth outside the polar regions. The Siachen Glacier (long) and Biafo Glacier (long) are the second- and third-longest glaciers outside the polar regions.[6]

The Karakoram is bounded on the east by the Aksai Chin plateau, on the northeast by the edge of the Tibetan Plateau and on the north by the river valleys of the Yarkand and Karakash rivers beyond which lie the Kunlun Mountains. At the northwest corner are the Pamir Mountains. The southern boundary of the Karakoram is formed, west to east, by the Gilgit, Indus and Shyok rivers, which separate the range from the northwestern end of the Himalaya range proper. These rivers flow northwest before making an abrupt turn southwestward towards the plains of Pakistan. Roughly in the middle of the Karakoram range is the Karakoram Pass, which was part of a historic trade route between Ladakh and Yarkand that is now inactive.

The Tashkurghan National Nature Reserve and the Pamir Wetlands National Nature Reserve in the Karalorun and Pamir mountains have been nominated for inclusion in UNESCO in 2010 by the National Commission of the People's Republic of China for UNESCO and have been tentatively added to the list.[7]

Name

Karakoram is a Turkic term meaning black gravel. The Central Asian traders originally applied the name to the Karakoram Pass.[8] Early European travellers, 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.[9] Later terminology was influenced by the Survey of India, whose surveyor Thomas Montgomerie in the 1850s gave the labels K1 to K6 (K for Karakoram) to six high mountains visible from his station at Mount Haramukh in Kashmir Valley, codes extended further 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 Himalayas further east. European explorers first visited early in the 19th century, followed by British surveyors starting in 1856.

The Muztagh Pass was crossed in 1887 by the expedition of Colonel Francis Younghusband[10] and the valleys above the Hunza River 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 Baltoro Muztagh. The term is now used to refer to the entire range from the Batura Muztagh above Hunza in the west to the Saser Muztagh in the bend of the Shyok River 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.[11] [12]

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.[13] A significant part, somewhere between 28 and 50 percent, of the Karakoram Range is glaciated covering an area of more than 15000-2NaN-2,[14] compared to between 8 and 12 percent of the Himalaya and 2.2 percent of the Alps.[15] Mountain glaciers 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,[16] [17] [18] unlike the Himalayas where glaciers are losing mass at significantly higher rate, many Karakoram glaciers are covered in a layer of rubble which insulates the ice from the warmth of the sun.[19] Where there is no such insulation, the rate of retreat is high.[20]

Ice Age

In the last ice age, a connected series of glaciers stretched from western Tibet to Nanga Parbat, and from the Tarim basin to the Gilgit District.[21] [22] [23] To the south, the Indus glacier was the main valley glacier, which flowed 120km (80miles) down from Nanga Parbat massif to 870m (2,850feet) elevation.[24] In the north, the Karakoram glaciers joined those from the Kunlun Mountains and flowed down to 2000m (7,000feet) in the Tarim basin.[25]

While the current valley glaciers in the Karakoram reach a maximum length of 76km (47miles), several of the ice-age valley glacier branches and main valley glaciers, had lengths up to 700km (400miles). During the Ice Age, the glacier snowline was about 1300m (4,300feet) lower than today.

Highest peaks

Here is a list for the highest peaks of the Karakoram. Included are some of the mountains named with a K code, the most famous of which is the K2 (mountain).

MountainHeight[26] RankedK codeRemark
K28611m (28,251feet)2K2 at the head of the Godwin-Austen Glacier
Gasherbrum I8080m (26,510feet)11K5
Broad Peak8051m (26,414feet)12
Gasherbrum II8034m (26,358feet)13K4
Gasherbrum III7952m (26,089feet)K3a, not on world highest list
Gasherbrum IV7925m (26,001feet)17K3
Distaghil Sar7885m (25,869feet)19
Kunyang Chhish7852m (25,761feet)21
Masherbrum I7821m (25,659feet)22K1
Batura I7795m (25,574feet)25
Rakaposhi7788m (25,551feet)26
Batura II7762m (25,466feet), not on world highest list
Kanjut Sar7760m (25,460feet)28
Saltoro Kangri I7742m (25,400feet)31K10
Batura III7729m (25,358feet), not on world highest list
Saltoro Kangri II7705m (25,279feet)K11
Saser Kangri I7672m (25,171feet)35K22
Chogolisa7665m (25,148feet)36
Shispare Sar7611m (24,970feet)38
Trivor Sar7577m (24,859feet)39
Skyang Kangri7545m (24,754feet)43
Mamostong Kangri7516m (24,659feet)47K35
Saser Kangri II7513m (24,649feet)48
Saser Kangri III7495m (24,590feet)51
Pumari Chhish7492m (24,580feet)53
Passu Sar7478m (24,534feet)54
Yukshin Gardan Sar7469m (24,505feet)55
Teram Kangri I7462m (24,482feet)56
Malubiting7458m (24,469feet)58
K12 or Saitang Peak7428m (24,370feet)61K12 subsidiary of Saltoro Kangri
Sia Kangri7422m (24,350feet)63
Skilma Gangri or Ghursay Kangri II7422m (24,350feet)K8 on the western flank of the Siachen Glacier
Momhil Sar7414m (24,324feet)64
Skil Brum7410m (24,310feet)66
Haramosh Peak7409m (24,308feet)67
Ghent Kangri7401m (24,281feet)69
Ultar Peak7388m (24,239feet)70
Rimo I7385m (24,229feet)71
Sherpi Kangri7380m (24,210feet)74
Bojohagur Duanasir7329m (24,045feet), not on world highest list
Yazghil Dome South7324m (24,029feet), not on world highest list
Baltoro Kangri7312m (23,990feet)81
Crown Peak7295m (23,934feet)83
Baintha Brakk7285m (23,901feet)86
Yutmaru Sar7283m (23,894feet)87
Baltistan Peak7282m (23,891feet)88K6
Muztagh Tower7273m (23,862feet)90
Diran7266m (23,839feet)92
Apsarasas Kangri I7243m (23,763feet)95
Rimo III7233m (23,730feet)97
Gasherbrum V7147m (23,448feet), not on world highest list
Gamba Gangri7000m (23,000feet) (approx)K9 near Trango Towers
Gomgma Gangri6934m (22,749feet)K7 at the head of the Charakusa Valley
Dansam Peak6666m (21,870feet)K13 south west of Saltoro Kangri
Pastan Kangri6523m (21,401feet)K25 south of Saltoro Kangri

The majority of the highest peaks are in the Gilgit–Baltistan region administered by Pakistan. Baltistan has more than 100 mountain peaks exceeding 6100m (20,000feet) height from sea level.

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.[27] 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 novels and movies. Rudyard Kipling refers to the Karakoram mountain range in his novel Kim, which was first published in 1900. Marcel Ichac 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. Greg Mortenson details the Karakoram, and specifically K2 and the Balti, 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.[29]

See also

References

Sources

Further reading

External links

Notes and References

  1. .
  2. Web site: Hindu Kush Himalayan Region . . 2014-10-17.
  3. .
  4. Web site: The Eight-Thousanders . Voiland. Adam . 2013 . . 2016-12-23.
  5. . . Mountains . 3.
  6. 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, Swiss Foundation for Alpine Research, Zurich, 1990.
  7. Web site: Karakorum-Pamir . UNESCO . 16 February 2013.
  8. Book: Mason, Kenneth . Kenneth Mason (geographer) . Exploration of the Shaksgam Valley and Aghil ranges, 1926 . 1928 . 72 . 978-81-206-1794-0.
  9. Nomenclature in the Karakoram: Discussion . Close C, Burrard S, Younghusband F, etal . The Geographical Journal . 76 . 2 . 1930 . 148–158 . 10.2307/1783980 . 1783980 . Blackwell Publishing.
  10. [Patrick French|French, Patrick]
  11. Indigenous Uses, Population Density, and Conservation of Threatened Medicinal Plants in Protected Areas of the Indian Himalayas . Conservation Biology . 19 . 2 . 368–378 . 2005 . Chandra Prakash . Kala . 10.1111/j.1523-1739.2005.00602.x. 85324142 .
  12. Kala . Chandra Prakash . Health traditions of Buddhist community and role of amchis in trans-Himalayan region of India . Current Science . 89 . 8 . 2005 . 1331 .
  13. 10.3301/IJG.2011.08 . Geological evolution of the Karakoram ranges . Italian Journal of Geosciences . 130 . 2011 . 2 . 147–159.
  14. 10.1016/j.jhydrol.2019.04.057 . 2019JHyd..574..467M . Early twenty-first century glacier mass losses in the Indus Basin constrained by density assumptions . 2019 . Muhammad . Sher . Tian . Lide . Khan . Asif . Journal of Hydrology . 574 . 467–475 . free.
  15. Book: Gansser . 1975 . Geology of the Himalayas . Interscience Publishers . London.
  16. Web site: Debris on certain Himalayan glaciers may prevent melting . Gail . Gallessich . sciencedaily.com . 2011 . January 30, 2011.
  17. 10.1016/j.rse.2016.10.034 . 2016RSEnv.187..505M . Changes in the ablation zones of glaciers in the western Himalaya and the Karakoram between 1972 and 2015 . 2016 . Muhammad . Sher . Tian . Lide . Remote Sensing of Environment . 187 . 505–512 . free.
  18. 10.1017/jog.2019.5 . 2019JGlac..65..270M . No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016 . 2019 . Muhammad . Sher . Tian . Lide . Nüsser . Marcus . Journal of Glaciology . 65 . 250 . 270–278 . free.
  19. 10.1016/j.scitotenv.2020.141119 . Thin debris layers do not enhance melting of the Karakoram glaciers . 2020 . Science of the Total Environment . 746 . 141119 . 32763605 . 2020ScTEn.746n1119M . free. Muhammad . Sher . Tian . Lide . Ali . Shaukat . Latif . Yasir . Wazir . Muhammad Atif . Goheer . Muhammad Arif . Saifullah . Muhammad . Hussain . Iqtidar . Shiyin . Liu .
  20. A Remote sensing approach for monitoring debris-covered glaciers in the high altitude Karakoram Himalayas . B.K. . Veettil . International Journal of Geomatics and Geosciences . 2012 . 2 . 833–841 . 3.
  21. Kuhle . M. . 1988 . The Pleistocene Glaciation of Tibet and the Onset of Ice Ages- An Autocycle Hypothesis.Tibet and High Asia. Results of the Sino-German Joint Expeditions (I) . GeoJournal . 17 . 4 . 581–596 . 10.1007/BF00209444 . 129234912.
  22. Book: Kuhle, M. . 2006 . The Past Hunza Glacier in Connection with a Pleistocene Karakoram Ice Stream Network during the Last Ice Age (Würm) . Kreutzmann . H. . Saijid . A. . Karakoram in Transition . Karachi, Pakistan . Oxford University Press . 24–48.
  23. Book: Kuhle, M. . 2011 . The High Glacial (Last Ice Age and Last Glacial Maximum) Ice Cover of High and Central Asia, with a Critical Review of Some Recent OSL and TCN Dates . Ehlers . J. . Gibbard . P.L. . Hughes . P.D. . Quaternary Glaciation – Extent and Chronology, A Closer Look . Amsterdam . Elsevier BV . 943–965. (glacier maps downloadable)
  24. Kuhle . M. . 2001 . Tibet and High Asia (VI): Glaciogeomorphology and Prehistoric Glaciation in the Karakoram and Himalaya . GeoJournal . 54 . 1–4 . 109–396 . 10.1023/A:1021307330169.
  25. Kuhle . M. . 1994 . Present and Pleistocene Glaciation on the North-Western Margin of Tibet between the Karakoram Main Ridge and the Tarim Basin Supporting the Evidence of a Pleistocene Inland Glaciation in Tibet. Tibet and High Asia. Results of the Sino-German and Russian-German Joint Expeditions (III) . GeoJournal . 33 . 133–272 . 2/3 . 10.1007/BF00812877. 189882345 .
  26. For Nepal, the heights indicated on the Nepal Topographic Maps are followed. For China and the Baltoro Karakoram, the heights are those of Mi Desheng's "The Maps of Snow Mountains in China". For the Hispar Karakoram the heights on a Russian 1:100,000 topo map of Web site: Hispar area expeditions . dead . https://web.archive.org/web/20080427142155/http://echidna.rutgers.edu/expeditions/Hispar/Default.htm . 2008-04-27 . 2008-07-15. seem to be more accurate than the customarily quoted heights probably based on US army maps from the 50s http://viewfinderpanoramas.org/elevmisquotes.html#hispar. Elsewhere, unless otherwise indicated, heights are those in Jill Neate's "High Asia".
  27. Jerzy Wala, Orographical Sketch Map of the Karakoram, Swiss Foundation for Alpine Research, Zurich, 1990.
  28. Web site: Naltar Valley: Heaven on Earth . shuaib . 2019-08-18 . Mehmaan Resort . en-US . 2019-09-01 . 1 September 2019 . https://web.archive.org/web/20190901082129/https://mehmaanresort.pk/naltar-valley-heaven-on-earth/ . dead .
  29. Book: Tarar, Mustansar Hussain . 1994 . K2 kahani . Lahore . Sang-e-Meel (published in Urdu) . 179 . 969-35-0523-9 . 18941738M.