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Pamir Mountains
Pamir Mountains
Highest point
Peak	Kongur Tagh
Elevation	7,649 m (25,095 ft)
Coordinates	38°35′39″N 75°18′48″E / 38.59417°N 75.31333°E / 38.59417; 75.31333
Geography
Countries	Tajikistan Kyrgyzstan Afghanistan China Pakistan
States/Provinces	Gorno-Badakhshan Osh Region Wakhan Chitral Gilgit Baltistan Xinjiang
Range coordinates	38°30′N 73°30′E / 38.5°N 73.5°E / 38.5; 73.5

The Pamir Mountains are a range of mountains between Central Asia and South Asia. They are located at a junction with other notable mountains, namely the Tian Shan, Karakoram, Kunlun, Hindu Kush and the Himalaya mountain ranges. They are among the world's highest mountains.

Much of the Pamir Mountains lie in the Gorno-Badakhshan region of Tajikistan. Spanning the border parts of four countries, to the south, they border the Hindu Kush mountains along Afghanistan's Wakhan Corridor in Badakhshan Province, Chitral and Gilgit-Baltistan regions of Pakistan. To the north, they join the Tian Shan mountains along the Alay Valley of Kyrgyzstan. To the east, they extend to the range that includes China's Kongur Tagh, in the "Eastern Pamirs", separated by the Yarkand valley from the Kunlun Mountains.

Since the Victorian era, they have been known as the "Roof of the World", presumably a translation from Persian.

Names and etymology

In other languages

The Pamir region is home to several different cultures, peoples and languages. In some of these languages, the Pamir Mountains are referred by different names.

In Indo-European languages, they are called:

• پامیر غرونه Pāmīr Ghrūna in Pashto;
• رشته کوه‌های پامیر, Ришта Кӯҳҳои Помир, Rishta Kūhhoi Pomir in Tajik;
• پامیر کوهستان Pāmīr Kohistān in Urdu;
• सुमेरु Sumeru in Sanskrit.

In Turkic languages, they are called:

• پامىر توولورۇ, Памир Тоолору, Pamir Tooloru in Kyrgyz;
• پامىر ئېگىزلىكى, Pamir Ëgizliki, Памир Егизлики in Uyghur.

In Chinese, they are referred as "Onion Range" (simplified Chinese: 葱岭; traditional Chinese: 蔥嶺; pinyin: Cōnglǐng; Wade–Giles: Ts'ung-ling), which is named after the wild onions growing in the region; In the Dungan dialect of Mandarin, it is written Памир / Цунлин in the Cyrillic alphabet, and in Xiao'erjing it is written پَامِعَر / ڞوْلٍْ. The name "Pamir" is used more commonly in Modern Chinese and loaned as 帕米尔 / 帕米爾 Pàmǐ'ěr.

Geological term

According to Middleton and Thomas, "pamir" is also a geological term. A pamir is a flat plateau or U-shaped valley surrounded by mountains. It forms when a glacier or ice field melts leaving a rocky plain. A pamir lasts until erosion forms soil and cuts down normal valleys. This type of terrain is found in the east and north of the Wakhan, and the east and south of Gorno-Badakhshan, as opposed to the valleys and gorges of the west. Pamirs are used for summer pasture.

The Great Pamir is around Lake Zorkul. The Little Pamir is east of this in the far east of Wakhan. The Taghdumbash Pamir is between Tashkurgan and the Wakhan west of the Karakoram Highway. The Alichur Pamir is around Yashil Kul on the Gunt River. The Sarez Pamir is around the town of Murghab, Tajikistan. The Khargush Pamir is south of Lake Karakul. There are several others.

The Pamir River is in the south-west of the Pamirs.

Geography

• Kongur Tagh (left) and Kongur Tiube (slightly to the right) as seen from the Karakoram Highway
• Slopes of Pamir Mountains on the Chinese side and Muztagh Ata
• Pamir Mountains from a NASA satellite image, April 2012

Mountain

The three highest mountains in the Pamirs core are Ismoil Somoni Peak (known from 1932 to 1962 as Stalin Peak, and from 1962 to 1998 as Communism Peak), 7,495 m (24,590 ft); Ibn Sina Peak (still unofficially known as Lenin Peak), 7,134 m (23,406 ft); and Peak Korzhenevskaya (Russian: Пик Корженевской, Pik Korzhenevskoi), 7,105 m (23,310 ft). In the Eastern Pamirs, China's Kongur Tagh is the highest at 7,649 m (25,095 ft).

Among the significant peaks of the Pamir Mountains are the following:

Name	Height in meters	Coord.	Sub-range	Country
Kongur (Kungur Tagh)	7,649	(38°35′36″N 75°18′45″E / 38.593428°N 75.312560°E / 38.593428; 75.312560 (Kongur))	Kongur Shan	China
Kongur Jiubie (Kungur Tjube Tagh)	7,530	(38°36′57″N 75°11′45″E / 38.615833°N 75.195833°E / 38.615833; 75.195833 (Kungur Tjube Tagh))	Kongur Shan	China
Muztagh Ata	7,509	(38°16′33″N 75°06′58″E / 38.275855°N 75.1161°E / 38.275855; 75.1161 (Muztagata))	Muztagh Ata Massif	China
Ismoil Somoni Peak (formerly Communism Peak, Stalin Peak)	7,495	(38°56′36″N 72°00′57″E / 38.943422°N 72.015803°E / 38.943422; 72.015803 (Ismoil Somoni Peak))	Academy of Sciences Range	Tajikistan
Lenin Peak (new name: Abu Ali Ibn Sino Peak; formerly Kaufmann Peak)	7,134	(39°20′37″N 72°52′39″E / 39.343724°N 72.877536°E / 39.343724; 72.877536 (Pik Lenin))	Trans-Alay Range	Tajikistan,  Kyrgyzstan
Peak Korzhenevskaya	7,105	(39°03′26″N 72°00′35″E / 39.057317°N 72.00983°E / 39.057317; 72.00983 (Peak Korzhenevskaya))	Academy of Sciences Range	Tajikistan
Independence Peak (also Qullai Istiqlol, formerly Revolution Peak, Dreispitz)	6,940	(38°30′36″N 72°21′15″E / 38.51°N 72.354167°E / 38.51; 72.354167 (Independence Peak))	Yazgulem Range	Tajikistan
Russia Peak	6,875	(38°53′46″N 72°01′44″E / 38.896°N 72.029°E / 38.896; 72.029 (Russia Peak))	Academy of Sciences Range	Tajikistan
Moscow Peak	6,785	(38°56′55″N 71°50′04″E / 38.948563°N 71.8344°E / 38.948563; 71.8344 (Moscow Peak))	Peter I Range	Tajikistan
Karl Marx Peak	6,726	(37°09′45″N 72°28′54″E / 37.1625°N 72.481667°E / 37.1625; 72.481667 (Karl Marx Peak))	Shakhdara Range	Tajikistan
Gora Kurumdy	6,614	(39°27′21″N 73°34′01″E / 39.455812°N 73.566978°E / 39.455812; 73.566978 (Gora Kurumdy))	Trans-Alay Range	Tajikistan,  Kyrgyzstan
Mount Garmo	6,595	(38°48′39″N 72°04′20″E / 38.810955°N 72.072344°E / 38.810955; 72.072344 (Mount Garmo))	Academy of Sciences Range	Tajikistan
Engels Peak	6,510	(37°10′18″N 72°31′22″E / 37.171671°N 72.522898°E / 37.171671; 72.522898 (Engels Peak))	Shakhdara Range	Tajikistan
Kohi Pamir	6,320	(37°09′N 73°13′E / 37.15°N 73.21°E / 37.15; 73.21 (Koh-e Pamir))	Wakhan Range	Afghanistan
Peak of the Soviet Officers	6,233	(38°25′26″N 73°18′07″E / 38.424°N 73.302°E / 38.424; 73.302 (Peak of the Soviet Officers))	Muzkol Range	Tajikistan
Mayakovskiy Peak	6,095	(37°01′16″N 71°42′54″E / 37.021092°N 71.715138°E / 37.021092; 71.715138 (Mayakovskiy Peak))	Shakhdara Range	Tajikistan
Patkhor Peak	6,083	(37°53′21″N 72°11′21″E / 37.889167°N 72.189167°E / 37.889167; 72.189167 (Patkhor Peak))	Rushan Range	Tajikistan
Leipzig Peak	5,725	(39°20′53″N 72°28′37″E / 39.348°N 72.477°E / 39.348; 72.477 (Leipzig Peak))	Trans-Alay Range	Tajikistan,  Kyrgyzstan
Skalisty Peak (Schugnan Range)	5,707	(37°36′02″N 72°13′37″E / 37.6005°N 72.227°E / 37.6005; 72.227 (Skalisty Peak))	Schugnan Range	Tajikistan
Kysyldangi Peak	5,704	(37°24′02″N 72°50′37″E / 37.4006°N 72.8435°E / 37.4006; 72.8435 (Kysyldangi Peak))	Southern Alitschur Range	Tajikistan

Remark: The summits of the Kongur and Muztagata Group are in some sources counted as part of the Kunlun, which would make Pik Ismoil Somoni the highest summit of the Pamir.

Glaciers

There are many glaciers in the Pamir Mountains, including the 77 km (48 mi) long Fedchenko Glacier, the longest in the former USSR and the longest glacier outside the polar regions. Approximately 12,500 km (ca. 10%) of the Pamirs are glaciated. Glaciers in the Southern Pamirs are retreating rapidly. Ten percent of annual runoff is supposed to originate from retreating glaciers in the Southern Pamirs. In the North-Western Pamirs, glaciers have almost stable mass balances.

Climate

Covered in snow during most of the year, the Pamirs have long and bitterly cold winters, and short, cool summers, which equals an ET (tundra climate) according to Köppen climate classification (EF above the snow line). Annual precipitation is about 130 mm (5 in), which supports grasslands but few trees.

Paleoclimatology during the Ice Age

The East-Pamir, in the centre of which the massifs of Mustagh Ata (7620 m) and Kongur Tagh (Qungur Shan, 7578, 7628 or 7830 m) are situated, shows from the western margin of the Tarim Basin an east–west extension of c. 200 km. Its north–south extension from King Ata Tagh up to the northwest Kunlun foothills amounts to c.170 km. Whilst the up to 21 km long current valley glaciers are restricted to mountain massifs exceeding 5600 m in height, during the last glacial period the glacier ice covered the high plateau with its set-up highland relief, continuing west of Mustagh Ata and Kongur. From this glacier area an outlet glacier has flowed down to the north-east through the Gez valley up to c.1850 m asl (meters above sea level) and thus as far as to the margin of the Tarim basin. This outlet glacier received inflow from the Kaiayayilak glacier from the Kongur north flank. From the north-adjacent Kara Bak Tor (Chakragil, c. 6800 or 6694 m) massif, the Oytag valley glacier in the same exposition flowed also down up to c. 1850 m asl. At glacial times the glacier snowline (ELA) as altitude limit between glacier nourishing area and ablation zone, was about 820 to 1250 metres lower than it is today. Under the condition of comparable proportions of precipitation there results from this a glacial depression of temperature of at least 5 to 7.5 °C.

Economy

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

Exploration

The lapis lazuli found in Egyptian tombs is thought to come from the Pamir area in Badakhshan province of Afghanistan. About 138 BCE Zhang Qian reached the Fergana Valley northwest of the Pamirs. Ptolemy vaguely describes a trade route through the area. From about 600 CE, Buddhist pilgrims travelled on both sides of the Pamirs to reach India from China. In 747 a Tang army was on the Wakhan River. There are various Arab and Chinese reports. Marco Polo may have travelled along the Panj River. In 1602 Bento de Goes travelled from Kabul to Yarkand and left a meager report on the Pamirs. In 1838 Lieutenant John Wood reached the headwaters of the Pamir River. From about 1868 to 1880, a number of Indians in the British service secretly explored the Panj area. In 1873 the British and Russians agreed to an Afghan frontier along the Panj River. From 1871 to around 1893 several Russian military-scientific expeditions mapped out most of the Pamirs (Alexei Pavlovich Fedchenko, Nikolai Severtzov, Captain Dmitry Putyata and others. Later came Nikolai Korzhenevskiy). Several local groups asked for Russian protection from Afghan raiders. The Russians were followed by a number of non-Russians including Ney Elias, George Littledale, the Earl of Dunmore, Wilhelm Filchner and Lord Curzon who was probably the first to reach the Wakhan source of the Oxus River. In 1891 the Russians informed Francis Younghusband that he was on their territory and later escorted a Lieutenant Davidson out of the area ('Pamir Incident'). In 1892 a battalion of Russians under Mikhail Ionov entered the area and camped near the present Murghab. In 1893 they built a proper fort there (Pamirskiy Post). In 1895 their base was moved to Khorog facing the Afghans.

In 1928 the last blank areas around the Fedchenko Glacier were mapped by a German-Soviet expedition under Willi Rickmer Rickmers.

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.

The earliest known evidence of human cannabis use was found in tombs at the Jirzankal Cemetery.

Transport

The Pamir Highway, the world's second highest international road, runs from Dushanbe in Tajikistan to Osh in Kyrgyzstan through the Gorno-Badakhshan Autonomous Province, and is the isolated region's main supply route. The Great Silk Road crossed a number of Pamir Mountain ranges.

Tourism

In December 2009, the New York Times featured articles on the possibilities for tourism in the Pamir area of Tajikistan. 2013 proved to be the most successful year ever for tourism in the region and tourism development continues to be the fastest growing economic sector.

Strategic position

Historically, the Pamir Mountains were considered a strategic trade route between Kashgar and Kokand on the Northern Silk Road, a prehistoric trackway, and have been subject to numerous territorial conquests. The Northern Silk Road (about 2,600 km (1,616 mi) in length) connected the ancient Chinese capital Chang'an with Kashgar over the Pamir Mountains towards the west, and from there continued to ancient Parthia. In the 20th century, these mountains have been the setting for the Tajikistan Civil War, border disputes between China and the Soviet Union, establishment of military bases by the US, Russia, and India, and renewed interest in trade development and resource exploration. The Chinese government says it has resolved most of the disputes it had with Central Asian countries.

Religious symbolism

Some researchers identify the Pamirs with the Mount Meru or Sumeru. The Mount Meru is the sacred five-peaked mountain of Buddhist and Jain, and is considered to be the center of all the physical, metaphysical and spiritual universes.

See also

• Tajik National Park
• Pamir languages
• Pamiris
• List of mountain ranges
• List of highest mountains
• Soviet Central Asia
• Central Asia
• Mount Imeon
• Ak-Baital Pass
• China–Tajikistan border
• Karachukar Valley

Notes

1. Also claimed by the Republic of China on Taiwan as part of Sinkiang Province.
2. The snow line that separates the snow above from the firn (1 yr old snow) or bare glacier ice below is the equilibrium line altitude (ELA).

References

1. According to the Big Soviet Encyclopedia "The question of the natural boundaries of Pamir is debatable. Normally Pamir is regarded as covering the territory from Trans-Alay Range to the north, Sarykol Range to the east, Lake Zorkul, Pamir River, and the upper reaches of Panj River to the south, and the meridional section of the Panj valley to the west; to the north-west Pamir includes the eastern parts of Peter the Great and Darvaz ranges."
2. "Pamirs summary - Britannica". Encyclopædia Britannica. 2 May 2020. Retrieved 27 October 2024.
3. Arnaud, N. O.; Brunel, M.; Cantagrel, J. M.; Tapponnier, P. (1993). "High cooling and denudation rates at Kongur Shan, Eastern Pamir (Xinjiang, China)". Tectonics. 12 (3): 1335–1346. doi:10.1029/93TC00767.
4. Bliss, Frank (2002-06-01). Social and Economic Change in the Pamirs (Gorno-Badakhshan, Tajikistan): Translated from German by Nicola Pacult and Sonia Guss with support of Tim Sharp. Taylor & Francis. pp. 13–14. ISBN 978-0-203-40531-4. Pamir = a Persian compilation of pay-I-mehr, the "roof of the world".
5. Li, Daoyuan. 水經注  [Commentary on the Water Classic] (in Chinese). Vol. 2 – via Wikisource. 蔥嶺在敦煌西八千里，其山高大，上生蔥，故曰蔥嶺也。(quoting from the "西河舊事") The Onion Range is 8,000 Li west of Dunhuangin Uzbek Language "Pamir Tog'i". Its mountains are high and onions grow on them, therefore it is called Onion Range.
6. "The origin of the Chinese name "Onion Range" for Pamir". Depts.washington.edu. 2002-04-14. Retrieved 2009-08-10.
7. ^ This section is based on the book by R. Middleton and H. Thomas: Robert Middleton and Huw Thomas, 'Tajikistan and the High Pamirs', Odyssey Books, 2008
8. ^ "Aga Khan Development Network (2010): Wakhan and the Afghan Pamir" (PDF). p. 3. Archived from the original (PDF) on 2011-12-25.
9. Tajikistan: 15 Years of Independence, statistical yearbook, Dushanbe, 2006, p. 8, in Russian.
10. "Dominance". www.8000ers.com. Retrieved 6 April 2010.
11. In the Karakoram Mountains, Siachen Glacier is 76 km long, Biafo Glacier is 67 km long, and Baltoro is 63 km long. The Bruggen or Pio XI Glacier in southern Chile is 66 km long. Kyrgyzstan's South Inylchek (Enylchek) Glacier is 60.5 km in length. Measurements are from recent imagery, generally with Russian 1:200,000 scale topographic mapping for reference as well as the 1990 Orographic Sketch Map: Karakoram: Sheets 1 and 2, Swiss Foundation for Alpine Research, Zurich.
12. ^ Knoche, Malte; Merz, Ralf; Lindner, Martin; Weise, Stephan M. (2017-06-13). "Bridging Glaciological and Hydrological Trends in the Pamir Mountains, Central Asia". Water. 9 (6): 422. doi:10.3390/w9060422.
13. "Mendenhall Glacier Facts" (PDF). University of Alaska Southeast. Juneau, Alaska, US: University of Alaska Southeast. 29 April 2011. p. 2. Archived from the original (PDF) on December 8, 2015. Retrieved 24 February 2019.
14. Kuhle, M. (1997):New findings concerning the Ice Age (LGM) glacier cover of the East Pamir, of the Nanga Parbat up to the Central Himalaya and of Tibet, as well as the Age of the Tibetan Inland Ice. Tibet and High Asia (IV). Results of Investigations into High Mountain Geomorphology. Paleo-Glaciology and Climatology of the Pleistocene. GeoJournal, 42, (2–3), pp. 87–257.
15. Kuhle, M. (2004):The High Glacial (Last Ice Age and LGM) glacier cover in High- and Central Asia. Accompanying text to the mapwork in hand with detailed references to the literature of the underlying empirical investigations. Ehlers, J., Gibbard, P. L. (Eds.). Extent and Chronology of Glaciations, Vol. 3 (Latin America, Asia, Africa, Australia, Antarctica). Amsterdam, Elsevier B.V., pp. 175–199.
16. Ren, Meng; Tang, Zihua; Wu, Xinhua; Spengler, Robert; Jiang, Hongen; Yang, Yimin; Boivin, Nicole (2019-06-07). "The origins of cannabis smoking: Chemical residue evidence from the first millennium BCE in the Pamirs". Science Advances. 5 (6): eaaw1391. Bibcode:2019SciA....5.1391R. doi:10.1126/sciadv.aaw1391. ISSN 2375-2548. PMC 6561734. PMID 31206023.
17. "Official Website of Pamir Travel". Pamir Travel. Archived from the original on 2007-09-28. Retrieved 2007-08-03.
18. "The Pamir Mountains of Tajikistan". The New York Times. 29 April 2011. Retrieved 2015-01-08.
19. Isaacson, Andy (17 December 2009). "Pamir Mountains, the Crossroads of History". The New York Times. Archived from the original on 2014-08-11.
20. "Silk Road, North China, C.Michael Hogan, the Megalithic Portal, ed. A. Burnham". Megalithic.co.uk. Retrieved 2009-08-10.
21. "India's 'Pamir Knot'". The Hindu. 11 November 2003. Archived from the original on 2007-12-10. Retrieved 2007-08-03.
22. "The West Is Red". Time. Archived from the original on February 11, 2009. Retrieved 2007-08-26.
23. "Huge Market Potential at China-Pakistan Border". China Daily. Retrieved 2007-08-26.
24. "China's Territorial and Boundary Affairs". Ministry of Foreign Affairs, the People's Republic of China. 2003-06-30. Retrieved 2017-02-05.
25. Chapman, Graham P. (2003). The Geopolitics of South Asia: From Early Empires to the Nuclear Age. Ashgate Publishing. p. 16. ISBN 9781409488071.
26. George Nathaniel Curzon; The Hindu World: An Encyclopedic Survey of Hinduism, 1968, p 184
27. Benjamin Walker - Hinduism; Ancient Indian Tradition & Mythology: Purāṇas in Translation, 1969, p 56
28. Jagdish Lal Shastri, Arnold Kunst, G. P. Bhatt, Ganesh Vasudeo Tagare - Oriental literature; Journal of the K.R. Cama Oriental Institute, 1928, p 38
29. Bernice Glatzer Rosenthal - History; Geographical Concepts in Ancient India, 1967, p 50
30. Bechan Dube - India; Geographical Data in the Early Purāṇas: A Critical Study, 1972, p 2
31. Dr M. R. Singh - India; Studies in the Proto-history of India, 1971, p 17
32. Gopal, Madan (1990). K.S. Gautam (ed.). India through the ages. Publication Division, Ministry of Information and Broadcasting, Government of India. p. 78.

Further reading

• Leitner, G. W. (1890). Dardistan in 1866, 1886 and 1893: Being an Account of the History, Religions, Customs, Legends, Fables and Songs of Gilgit, Chilas, Kandia (Gabrial) Yasin, Chitral, Hunza, Nagyr and other parts of the Hindukush. With a supplement to the second edition of The Hunza and Nagyr Handbook. And an Epitome of Part III of the author's “The Languages and Races of Dardistan”. First Reprint 1978. Manjusri Publishing House, New Delhi.
• Murray, Charles (1894). The Pamirs; being a narrative of a year's expedition on horseback and on foot through Kashmir, western Tibet, Chinese Tartary, and Russian Central Asia. J. Murray. (Vol. I and II)
• Curzon, George Nathaniel. (1896). The Pamirs and the Source of the Oxus. Royal Geographical Society, London. Reprint: Elibron Classics Series, Adamant Media Corporation. 2005. ISBN 1-4021-5983-8 (pbk; ISBN 1-4021-3090-2 (hbk).
• Wood, John, (1872). A Journey to the Source of the River Oxus. With an essay on the Geography of the Valley of the Oxus by Colonel Henry Yule. London: John Murray.
• Gordon, T. E. (1876). The Roof of the World: Being the Narrative of a Journey over the high plateau of Tibet to the Russian Frontier and the Oxus sources on Pamir. Edinburgh. Edmonston and Douglas. Reprint by Ch’eng Wen Publishing Company. Taipei. 1971.
• Cobbold, Ralph Patteson (1900). Innermost Asia: travel & sport in the Pamirs. W. Heinemann.
• Strong, Anna Louise. (1930). The Road to the Grey Pamir. Robert M. McBride & Co., New York.
• Toynbee, Arnold J. (1961). Between Oxus and Jumna. London. Oxford University Press.
• Slesser, Malcolm (1964). Red Peak: A Personal Account of the British-Soviet Expedition. Coward McCann.
• Wang, Miao (1983). From the Pamirs to Beijing : tracing Marco Polo's northern route. HK China Tourism Press.
• Tilman, H. W. (1983). "Two Mountains and a River" part of The Severn Mountain Travel Books. Diadem, London.
• Waugh, Daniel C. (1999). "The ‘Mysterious and Terrible Karatash Gorges’: Notes and Documents on the Explorations by Stein and Skrine." The Geographical Journal, Vol. 165, No. 3. (Nov., 1999), pp. 306–320.
• Horsman, S. (2002). Peaks, Politics and Purges: the First Ascent of Pik Stalin in Douglas, E. (ed.) Alpine Journal 2002 (Volume 107), The Alpine Club & Ernest Press, London, pp 199–206.
• Gecko-Maps (2004). The Pamirs. 1:500.000 – A tourist map of Gorno-Badkshan-Tajikistan and background information on the region. Verlag "Gecko-Maps", Switzerland (ISBN 3-906593-35-5)
• Dagiev, Dagikhudo, and Carole Faucher, eds. (2018). Identity, History and Trans-nationality in Central Asia: The Mountain Communities of Pamir. Routledge.

External links

• Life in Afghanistan's Pamir mountains
• Information and photos
• Afghan's Little Pamir – photos of the life of ethnic Kyrgyz (Archive)

v t e Mountain ranges of China
Geography of China
Northwestern	Altai Mountains Dzungarian Alatau Tian Shan Borohoro Mountains Tarbagatai Mountains Kunlun Mountains Altyn-Tagh Qilian Mountains Helan Mountains Liupan Mountains
Qinghai-Tibet and Southwestern	Himalayas Transhimalaya Pamir Mountains Karakoram Argu Tagh Yengisogat Kunlun Mountains Hoh Xil Bayan Har Mountains Amne Machin Tanggula Mountains Nyenchen Tanglha Mountains Hengduan Mountains Gaoligong Mountains Yunling Mountains Ailao Mountains Qionglai Mountains Daxue Mountains Min Mountains
Northeast	Greater Khingan Lesser Khingan Changbai Mountains Wanda Mountains Qian Mountains
North and East	Yin Mountains Lang Mountains Lüliang Mountains Taihang Mountains Zhongtiao Mountains Mount Tai Tianmu Mountain Yandang Mountains Wuyi Mountains
Central	Qinling Daba Mountains Dabie Mountains Wudang Mountains Jingshan Mountains Luoxiao Mountains Jiuling Mountains Mufu Mountains Wugong Mountains Huangshan Wuling Mountains Xuefeng Mountains
South	Cang Mountain Daliang Mountains Dalou Mountains Nanling Mountains Jiuyi Mountains Yuecheng Mountains Longmen Mountains Western Mountains
Landforms of China

• Pamir Mountains
• Landforms of Central Asia
• Mountain ranges of Asia
• Mountain ranges of China
• Mountain ranges of Afghanistan
• Mountain ranges of Pakistan
• Mountain ranges of Tajikistan
• Mountain ranges of Kyrgyzstan
• Physiographic provinces
• Landforms of Badakhshan Province