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Karakoram

Coordinates:36°N76°E/ 36°N 76°E/36; 76
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Karakoram
Baltoro Glacierin the Central KarakoramGilgit-Baltistan,Pakistan
Highest point
PeakK2
Elevation8,611 m (28,251 ft)
Coordinates35°52′57″N76°30′48″E/ 35.88250°N 76.51333°E/35.88250; 76.51333
Dimensions
Length500 km (310 mi)
Geography
Map
Interactive map outlining Karakoram range
CountriesAfghanistan,China,India,PakistanandTajikistan
Regions/ProvincesGilgit-Baltistan,Ladakh,XinjiangandBadakhshan
Range coordinates36°N76°E/ 36°N 76°E/36; 76
Borders onPamir Mountains,Hindu Kush,Kunlun Mountains,HimalayasandLadakh Range
Karakoram
Chinese name
ChineseKháchLạtCônLuânSơnMạch
Hanyu PinyinKālǎ Kūnlún shānmài
Literal meaning"Kara-Kunlun mountain range"
Tibetan name
Tibetanཁར་ཁོ་རུམ་རི
Uyghur name
Uyghurقاراقورام

TheKarakoram(/ˌkɑːrəˈkɔːrəm,ˌkær-/)[1]is amountain rangein theKashmirregion spanning the border ofPakistan,China,andIndia,with the northwestern extremity of the range extending toAfghanistanandTajikistan.Most of the Karakoram mountain range falls under the jurisdiction ofGilgit-Baltistan,which is controlled by Pakistan. Its highest (and theworld's second-highest) peak,K2,is located in Gilgit-Baltistan,Pakistan.It begins in theWakhan Corridor(Afghanistan) in the west, encompasses the majority of Gilgit-Baltistan, Pakistan and extends intoLadakh(controlled by India) andAksai Chin(controlled by China).

The Karakoram is thesecond-highest mountain rangeon Earth and part of a complex of ranges that includes thePamir Mountains,Hindu Kush,andHimalayas.[2][3]

The range contains 18 summits higher than 7,500 m (24,600 ft) inelevation,with four above 8,000 m (26,000 ft):[4][5][6]K2(8,611 m (28,251 ft)AMSL) (the second-highest peak on Earth),Gasherbrum I,Broad Peak,andGasherbrum II.

The range is about 500 km (311 mi) in length and is the mostglaciatedplace on Earth outside thepolar regions.TheSiachen Glacier(76 km (47 mi) long) andBiafo Glacier(63 km (39 mi) long) are the second- and third-longest glaciers outside the polar regions.[7]

The Karakoram is bounded on the east by theAksai Chinplateau, on the northeast by the edge of theTibetan Plateauand on the north by the river valleys of theYarkandandKarakash riversbeyond which lie theKunlun Mountains.At the northwest corner are thePamir Mountains.The southern boundary of the Karakoram is formed, west to east, by theGilgit,IndusandShyok rivers,which separate the range from the northwestern end of theHimalayarange proper. These rivers flow northwest before making an abrupt turn southwestward towards the plains ofPakistan.Roughly in the middle of the Karakoram range is theKarakoram Pass,which was part of a historic trade route betweenLadakhandYarkandthat is now inactive.

TheTashkurghan National Nature Reserveand thePamir Wetlands National Nature Reservein the Karalorun and Pamir mountains have been nominated for inclusion inUNESCOin 2010 by the National Commission of the People's Republic ofChinaforUNESCOand have been tentatively added to the list.[8]

Name[edit]

The black gravel of Karakoram mountains, as seen nearPakistan'sBiafo Glacier

Karakoram is aTurkicterm meaningblack gravel.The Central Asian traders originally applied the name to theKarakoram Pass.[9]Early European travellers, includingWilliam MoorcroftandGeorge Hayward,started using the term for the range of mountains west of the pass, although they also used the termMuztagh(meaning, "Ice Mountain" ) for the range now known as Karakoram.[9][10]Later terminology was influenced by theSurvey of India,whose surveyorThomas Montgomeriein the 1850s gave the labels K1 to K6 (K for Karakoram) to six high mountains visible from his station atMount HaramukhinKashmir Valley,codes extended further up to more than thirty.

In traditional Indian geography the mountains were known asKrishnagiri(black mountains),KanhagiriandKanheri.[11]

Exploration[edit]

Due to its altitude and ruggedness, the Karakoram is much less inhabited than parts of theHimalayasfurther east. European explorers first visited early in the 19th century, followed byBritish surveyorsstarting in 1856.

TheMuztagh Passwas crossed in 1887 by the expedition of ColonelFrancis Younghusband[12]and the valleys above theHunza Riverwere explored by General SirGeorge K. Cockerillin 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 byKenneth Mason,[9]for the range now known as theBaltoro Muztagh.The term is now used to refer to the entire range from theBatura MuztaghaboveHunzain the west to theSaser Muztaghin the bend of theShyok Riverin the east.

Hunza Valleyin theGilgit-Baltistanregion administered by Pakistan

Floral surveys were carried out in the Shyok River catchment and from Panamik to Turtuk village byChandra Prakash Kaladuring 1999 and 2000.[13][14]

Geology and glaciers[edit]

The Karakoram is in one of the world's most geologically active areas, at theplate boundary between the Indo-Australian plate and the Eurasian plate.[15] A significant part, somewhere between 28 and 50 percent, of the Karakoram Range is glaciated covering an area of more than 15,000 square kilometres or 5,800 square miles,[16]compared to between 8 and 12 percent of the Himalaya and 2.2 percent of theAlps.[17]Mountainglaciersmay serve as an indicator of climate change, advancing and receding with long-term changes in temperature and precipitation. The Karakoram glaciers are slightly retreating,[18][19][20]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.[21]Where there is no such insulation, the rate of retreat is high.[22]

Ice Age[edit]

In the lastice age,aconnected series of glaciersstretched from westernTibettoNanga Parbat,and from theTarim basinto theGilgit District.[23][24][25]To the south, theIndus glacierwas the main valley glacier, which flowed 120 kilometres (75 mi) down fromNanga Parbatmassif to 870 metres (2,850 ft) elevation.[23][26]In the north, the Karakoram glaciers joined those from theKunlun Mountainsand flowed down to 2,000 metres (6,600 ft) in the Tarim basin.[25][27]

While the current valley glaciers in the Karakoram reach a maximum length of 76 kilometres (47 mi), several of the ice-age valley glacier branches and main valley glaciers, had lengths up to 700 kilometres (430 mi). During the Ice Age, the glacier snowline was about 1,300 metres (4,300 ft) lower than today.[25][26]

Highest peaks[edit]

HighestKarakorampeaks in the Baltoro region as seen fromInternational Space Station
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75km
50miles
Gasherbrum V
48
Gasherbrum V
Rimo III
47
Rimo III
Apsarasas Kangri I
46
Apsarasas Kangri I
Diran
45
Diran
Muztagh Tower
44
Muztagh Tower
K6
43
K6
Yutmaru Sar
42
Yutmaru Sar
Baintha Brakk
41
Baintha Brakk
Crown Peak
40
Crown Peak
Baltoro Kangri
39
Baltoro Kangri
Yazghil Dome South
38
Yazghil Dome South
Sherpi Kangri
37
Sherpi Kangri
Rimo I
36
Rimo I
Ultar Sar
35
Ultar Sar
Ghent Kangri
34
Ghent Kangri
Haramosh Peak
33
Haramosh Peak
Skil Brum
32
Skil Brum
Momhil Sar
31
Momhil Sar
Sia Kangri
30
Sia Kangri
K12
29
K12
Malubiting
28
Malubiting
Teram Kangri I
27
Teram Kangri I
Yukshin Gardan Sar
26
Yukshin Gardan Sar
Passu Sar
25
Passu Sar
Pumari Chhish
24
Pumari Chhish
Saser Kangri III
23
Saser Kangri III
Saser Kangri II
22
Saser Kangri II
Mamostong Kangri K35
21
Mamostong Kangri K35
Skyang Kangri
20
Skyang Kangri
Trivor Sar
19
Trivor Sar
Shispare Sar
18
Shispare Sar
Chogolisa
17
Chogolisa
Saser Kangri I K22
16
Saser Kangri I K22
Batura III
15
Batura III
Saltoro Kangri K10
14
Saltoro Kangri K10
Kanjut Sar
13
Kanjut Sar
Batura II
12
Batura II
Rakaposhi
11
Rakaposhi
Batura I
10
Batura I
Masherbrum K1
9
Masherbrum K1
Khunyang Chhish
8
Khunyang Chhish
Distaghil Sar
7
Distaghil Sar
Gasherbrum IV K3
6
Gasherbrum IV K3
Gasherbrum III K3a
5
Gasherbrum III K3a
Gasherbrum II K4
4
Gasherbrum II K4
Broad Peak
3
Broad Peak
Gasherbrum I K5
2
Gasherbrum I K5
K2
1
K2
Location of the major peaks inKarakoram

Legend:
1:K2 2:Gasherbrum IK5 3:Broad Peak

4:Gasherbrum IIK4 5:Gasherbrum IIIK3a 6:Gasherbrum IVK3

7:Distaghil Sar 8:Khunyang Chhish 9:MasherbrumK1

10:Batura I 11:Rakaposhi 12:Batura II

13:Kanjut Sar 14:Saltoro KangriK10 15:Batura III

16:Saser Kangri IK22 17:Chogolisa 18:Shispare Sar

19:Trivor Sar 20:Skyang Kangri 21:Mamostong KangriK35

22:Saser Kangri II 23:Saser Kangri III 24:Pumari Chhish

25:Passu Sar 26:Yukshin Gardan Sar 27:Teram Kangri I

28:Malubiting 29:K12 30:Sia Kangri

31:Momhil Sar 32:Skil Brum 33:Haramosh Peak

34:Ghent Kangri 35:Ultar Sar 36:Rimo I

37:Sherpi Kangri 38:Yazghil Dome South 39:Baltoro Kangri

40:Crown Peak 41:Baintha Brakk 42:Yutmaru Sar

43:K6 44:Muztagh Tower 45:Diran

46:Apsarasas Kangri I 47:Rimo III 48:Gasherbrum V



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 theK2 (mountain).

Mountain Height[28] Ranked K code Remark
K2 8,611 metres (28,251 ft) 2 K2 ChinaPakistanat the head of the Godwin-Austen Glacier
Gasherbrum I 8,080 metres (26,510 ft) 11 K5 ChinaPakistan
Broad Peak 8,051 metres (26,414 ft) 12 ChinaPakistan
Gasherbrum II 8,034 metres (26,358 ft) 13 K4 ChinaPakistan
Gasherbrum III 7,952 metres (26,089 ft) K3a Pakistan,not on world highest list
Gasherbrum IV 7,925 metres (26,001 ft) 17 K3 Pakistan
Distaghil Sar 7,885 metres (25,869 ft) 19 Pakistan
Kunyang Chhish 7,852 metres (25,761 ft) 21 Pakistan
Masherbrum I 7,821 metres (25,659 ft) 22 K1 Pakistan
Batura I 7,795 metres (25,574 ft) 25 Pakistan
Rakaposhi 7,788 metres (25,551 ft) 26 Pakistan
Batura II 7,762 metres (25,466 ft) Pakistan,not on world highest list
Kanjut Sar 7,760 metres (25,460 ft) 28 Pakistan
Saltoro KangriI 7,742 metres (25,400 ft) 31 K10 IndiaPakistan
Batura III 7,729 metres (25,358 ft) Pakistan,not on world highest list
Saltoro KangriII 7,705 metres (25,279 ft) K11 IndiaPakistan
Saser KangriI 7,672 metres (25,171 ft) 35 K22 India
Chogolisa 7,665 metres (25,148 ft) 36 Pakistan
Shispare Sar 7,611 metres (24,970 ft) 38 Pakistan
TrivorSar 7,577 metres (24,859 ft) 39 Pakistan
Skyang Kangri 7,545 metres (24,754 ft) 43 ChinaPakistan
Mamostong Kangri 7,516 metres (24,659 ft) 47 K35 India
Saser KangriII 7,513 metres (24,649 ft) 48 India
Saser KangriIII 7,495 metres (24,590 ft) 51 India
Pumari Chhish 7,492 metres (24,580 ft) 53 Pakistan
Passu Sar 7,478 metres (24,534 ft) 54 Pakistan
Yukshin Gardan Sar 7,469 metres (24,505 ft) 55 Pakistan
Teram KangriI 7,462 metres (24,482 ft) 56 ChinaIndia
Malubiting 7,458 metres (24,469 ft) 58 Pakistan
K12orSaitang Peak 7,428 metres (24,370 ft) 61 K12 IndiaPakistansubsidiary ofSaltoro Kangri
Sia Kangri 7,422 metres (24,350 ft) 63 ChinaPakistan
Skilma Gangri or Ghursay Kangri II 7,422 metres (24,350 ft) K8 Pakistanon the western flank of theSiachen Glacier
Momhil Sar 7,414 metres (24,324 ft) 64 Pakistan
Skil Brum 7,410 metres (24,310 ft) 66 ChinaPakistan
Haramosh Peak 7,409 metres (24,308 ft) 67 Pakistan
Ghent Kangri 7,401 metres (24,281 ft) 69 IndiaPakistan
Ultar Peak 7,388 metres (24,239 ft) 70 Pakistan
Rimo I 7,385 metres (24,229 ft) 71 India
Sherpi Kangri 7,380 metres (24,210 ft) 74 Pakistan
Bojohagur Duanasir 7,329 metres (24,045 ft) Pakistan,not on world highest list
Yazghil Dome South 7,324 metres (24,029 ft) Pakistan,not on world highest list
Baltoro Kangri 7,312 metres (23,990 ft) 81 Pakistan
Crown Peak 7,295 metres (23,934 ft) 83 China
Baintha Brakk 7,285 metres (23,901 ft) 86 Pakistan
Yutmaru Sar 7,283 metres (23,894 ft) 87 Pakistan
Baltistan Peak 7,282 metres (23,891 ft) 88 K6 Pakistan
Muztagh Tower 7,273 metres (23,862 ft) 90 ChinaPakistan
Diran 7,266 metres (23,839 ft) 92 Pakistan
Apsarasas KangriI 7,243 metres (23,763 ft) 95 ChinaIndia
Rimo III 7,233 metres (23,730 ft) 97 India
Gasherbrum V 7,147 metres (23,448 ft) Pakistan,not on world highest list
Gamba Gangri 7,000 metres (23,000 ft) (approx) K9 PakistannearTrango Towers
Gomgma Gangri 6,934 metres (22,749 ft) K7 Pakistanat the head of theCharakusa Valley
Dansam Peak 6,666 metres (21,870 ft) K13 Pakistansouth west ofSaltoro Kangri
Pastan Kangri 6,523 metres (21,401 ft) K25 Indiasouth ofSaltoro Kangri

The majority of the highest peaks are in the Gilgit–Baltistan region administered by Pakistan. Baltistan has more than 100 mountain peaks exceeding 6,100 metres (20,000 ft) height from sea level.

Subranges[edit]

View of the Moon over Karakoram Range in Pakistan

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.[29]The ranges are listed roughly west to east.

Passes[edit]

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50miles
Kilik Pass
18
Kilik Pass
Mintaka Pass
17
Mintaka Pass
Mutsjliga Pass
16
Mutsjliga Pass
Khunjerab Pass
15
Khunjerab Pass
Sarpo Laggo Pass
14
Sarpo Laggo Pass
Mustagh Pass
13
Mustagh Pass
Windy Gap
12
Windy Gap
Turkistan La Pass
11
Turkistan La Pass
Karakoram Pass
10
Karakoram Pass
Shimshal Pass
9
Shimshal Pass
Hispar Pass
8
Hispar Pass
Naltar Pass
7
Naltar Pass
Machulo La
6
Machulo La
Burji La
5
Burji La
Sasser Pass
4
Sasser Pass
Gyong La
3
Gyong La
Bilafond La
2
Bilafond La
Sia La
1
Sia La

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[edit]

The Karakoram mountain range has been referred to in a number ofnovelsand movies.Rudyard Kiplingrefers to the Karakoram mountain range in his novelKim,which was first published in 1900.Marcel Ichacmade a film titledKarakoram,chronicling a French expedition to the range in 1936. The film won the Silver Lion at theVenice Film Festivalof 1937.Greg Mortensondetails the Karakoram, and specifically K2 and theBalti,extensively in his bookThree Cups of Tea,about his quest to build schools for children in the region.K2 Kahani(The K2 Story) byMustansar Hussain Tarardescribes his experiences at K2 base camp.[31]

See also[edit]

References[edit]

Citations[edit]

  1. ^"Karakoram".Dictionary.com Unabridged(Online). n.d.
  2. ^Karakoram Rangeat theEncyclopædia Britannica.
  3. ^"Hindu Kush Himalayan Region".International Centre for Integrated Mountain Development.Retrieved17 October2014.
  4. ^Shukurov, The Natural Environment of Central and South Asia 2005,p. 512.
  5. ^Voiland, Adam (2013)."The Eight-Thousanders".NASA Earth Observatory.Retrieved23 December2016.
  6. ^"Mountains".Planet Earth.Episode 3.BBC.
  7. ^Tajikistan's Fedchenko Glacier is 77 km (48 mi) long. Baltoro and Batura Glaciers in the Karakoram are 57 km (35 mi) 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.
  8. ^"Karakorum-Pamir".UNESCO.Retrieved16 February2013.
  9. ^abcMason, Kenneth(1928).Exploration of the Shaksgam Valley and Aghil ranges, 1926.p. 72.ISBN978-81-206-1794-0.
  10. ^Close C, Burrard S, Younghusband F, et al. (1930). "Nomenclature in the Karakoram: Discussion".The Geographical Journal.76(2). Blackwell Publishing: 148–158.doi:10.2307/1783980.JSTOR1783980.
  11. ^Kohli, M.S. (2002),Mountains of India: Tourism, Adventure and Pilgrimage,Indus Publishing, p. 22,ISBN978-81-7387-135-1
  12. ^French, Patrick.(1994).Younghusband: The Last Great Imperial Adventurer,pp. 53, 56-60. HarperCollinsPublishers,London. Reprint (1995): Flamingo. London.ISBN0-00-637601-0.
  13. ^Kala, Chandra Prakash (2005). "Indigenous Uses, Population Density, and Conservation of Threatened Medicinal Plants in Protected Areas of the Indian Himalayas".Conservation Biology.19(2): 368–378.doi:10.1111/j.1523-1739.2005.00602.x.S2CID85324142.
  14. ^Kala, Chandra Prakash (2005)."Health traditions of Buddhist community and role of amchis in trans-Himalayan region of India"(PDF).Current Science.89(8): 1331.
  15. ^"Geological evolution of the Karakoram ranges".Italian Journal of Geosciences.130(2): 147–159. 2011.doi:10.3301/IJG.2011.08.
  16. ^Muhammad, Sher; Tian, Lide; Khan, Asif (2019)."Early twenty-first century glacier mass losses in the Indus Basin constrained by density assumptions".Journal of Hydrology.574:467–475.Bibcode:2019JHyd..574..467M.doi:10.1016/j.jhydrol.2019.04.057.
  17. ^Gansser (1975).Geology of the Himalayas.London: Interscience Publishers.
  18. ^Gallessich, Gail (2011)."Debris on certain Himalayan glaciers may prevent melting".sciencedaily.com.Retrieved30 January2011.
  19. ^Muhammad, Sher; Tian, Lide (2016)."Changes in the ablation zones of glaciers in the western Himalaya and the Karakoram between 1972 and 2015".Remote Sensing of Environment.187:505–512.Bibcode:2016RSEnv.187..505M.doi:10.1016/j.rse.2016.10.034.
  20. ^Muhammad, Sher; Tian, Lide; Nüsser, Marcus (2019)."No significant mass loss in the glaciers of Astore Basin (North-Western Himalaya), between 1999 and 2016".Journal of Glaciology.65(250): 270–278.Bibcode:2019JGlac..65..270M.doi:10.1017/jog.2019.5.
  21. ^Muhammad, Sher; Tian, Lide; Ali, Shaukat; Latif, Yasir; Wazir, Muhammad Atif; Goheer, Muhammad Arif; Saifullah, Muhammad; Hussain, Iqtidar; Shiyin, Liu (2020)."Thin debris layers do not enhance melting of the Karakoram glaciers".Science of the Total Environment.746:141119.Bibcode:2020ScTEn.746n1119M.doi:10.1016/j.scitotenv.2020.141119.PMID32763605.
  22. ^Veettil, B.K. (2012). "A Remote sensing approach for monitoring debris-covered glaciers in the high altitude Karakoram Himalayas".International Journal of Geomatics and Geosciences.2(3): 833–841.
  23. ^abKuhle, 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.doi:10.1007/BF00209444.S2CID129234912.
  24. ^Kuhle, M. (2006). "The Past Hunza Glacier in Connection with a Pleistocene Karakoram Ice Stream Network during the Last Ice Age (Würm)". In Kreutzmann, H.; Saijid, A. (eds.).Karakoram in Transition.Karachi, Pakistan: Oxford University Press. pp. 24–48.
  25. ^abcKuhle, 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". In Ehlers, J.; Gibbard, P.L.; Hughes, P.D. (eds.).Quaternary Glaciation – Extent and Chronology, A Closer Look.Amsterdam: Elsevier BV. pp. 943–965.(glacier mapsdownloadable)
  26. ^abKuhle, M. (2001). "Tibet and High Asia (VI): Glaciogeomorphology and Prehistoric Glaciation in the Karakoram and Himalaya".GeoJournal.54(1–4): 109–396.doi:10.1023/A:1021307330169.
  27. ^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(2/3): 133–272.doi:10.1007/BF00812877.S2CID189882345.
  28. ^For Nepal, the heights indicated on the Nepal Topographic Maps are followed. For China and theBaltoroKarakoram, the heights are those of Mi Desheng's "The Maps of Snow Mountains in China". For theHispar Karakoramthe heights on a Russian 1:100,000 topo map of"Hispar area expeditions".Archived fromthe originalon 27 April 2008.Retrieved15 July2008.seem to be more accurate than the customarily quoted heights probably based on US army maps from the 50s[1].Elsewhere, unless otherwise indicated, heights are those in Jill Neate's "High Asia".
  29. ^Jerzy Wala,Orographical Sketch Map of the Karakoram,Swiss Foundation for Alpine Research, Zurich, 1990.
  30. ^shuaib (18 August 2019)."Naltar Valley: Heaven on Earth".Mehmaan Resort.Retrieved1 September2019.
  31. ^Tarar, Mustansar Hussain (1994).K2 kahani.Lahore: Sang-e-Meel (published in Urdu). p. 179.ISBN969-35-0523-9.OL18941738M.

Sources[edit]

Further reading[edit]

External links[edit]