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Coordinates: 39°00′N 92°00′E / 39.000°N 92.000°E / 39.000; 92.000
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Along the northern side of the mountains ran the main [[Silk road]] trade route from [[China proper]] to the Tarim Basin and westward. The Altun-Tagh and Qilians were sometimes called the [[Nan Shan]] ('south mountains') because they were south of the main route. Near the west end of the Altun-Shan the Gansu or [[Hexi corridor]] ends and the silk road splits. One branch follows the Altun-Tagh along the south side of the Tarim Basin while the other follows the north side.
Along the northern side of the mountains ran the main [[Silk road]] trade route from [[China proper]] to the Tarim Basin and westward. The Altun-Tagh and Qilians were sometimes called the [[Nan Shan]] ('south mountains') because they were south of the main route. Near the west end of the Altun-Shan the Gansu or [[Hexi corridor]] ends and the silk road splits. One branch follows the Altun-Tagh along the south side of the Tarim Basin while the other follows the north side.


The southwestern part of the Altyn-Tagh range reaches snowy peaks of up to 6295 m, although it descends to an average of 4000 m in the narrow middle and eventually rises up to average 5000 m as it meets the Nan Shan.
The southwestern part of the Altyn-Tagh range reaches snowy peaks of up to {{convert|6295|m|ft}}, although it descends to an average of {{convert|4000|m|ft}} in the narrow middle and eventually rises up to average {{convert|5000|m|ft}} as it meets the Nan Shan.


There are a dearth of rivers and streams in these mountains, due to the aridity of the region. The western portion has some small streams that either head north into the dessert or south into Lake Ayakkum. The remainder of the range is lacking in rivers.<ref name=EB/>
There are a dearth of rivers and streams in these mountains, due to the aridity of the region. The western portion has some small streams that either head north into the dessert or south into Lake Ayakkum. The remainder of the range is lacking in rivers.<ref name=EB/>
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Within southeastern Xinjiang, the main of these basins is the [[Kumkol Basin]] ({{zh|c=库木库里盆地|p=Kùmùkùlǐ Péndì}}){{refn|group=nb|The Chinese-based spelling ([[pinyin]]) for this place name, "Kumukuli Basin" is often used in English. When trying to produce a Turkic-like spelling for this name, authors occasionally transcribe it as "Kumukol Basin", as in the map in Fig. 2 in Meng & Fang's ''Cenozoic tectonic development of the Qaidam Basin in the northeastern Tibetan Plateau'',<ref>Meng, Qing-Ren; Fang, Xiang (2008) p. 3</ref> but more often as "Kumkol",<ref>Zheng, Mianping (1997) p. 229</ref> or "Kumkuli".}}
Within southeastern Xinjiang, the main of these basins is the [[Kumkol Basin]] ({{zh|c=库木库里盆地|p=Kùmùkùlǐ Péndì}}){{refn|group=nb|The Chinese-based spelling ([[pinyin]]) for this place name, "Kumukuli Basin" is often used in English. When trying to produce a Turkic-like spelling for this name, authors occasionally transcribe it as "Kumukol Basin", as in the map in Fig. 2 in Meng & Fang's ''Cenozoic tectonic development of the Qaidam Basin in the northeastern Tibetan Plateau'',<ref>Meng, Qing-Ren; Fang, Xiang (2008) p. 3</ref> but more often as "Kumkol",<ref>Zheng, Mianping (1997) p. 229</ref> or "Kumkuli".}}


The two main lakes in this basin are the saline [[Lake Aqqikkol]] (also Ajig Kum Kul,<ref>Holdich, Sir Thomas (2006); p. 228</ref> Achak-kum; {{zh|c=阿其克库勒湖|p= Āqíkèkùlè Hú}}; 37°05′N,88°25′E, 4,250 m elevation)<ref>www.baidu.com (2013)</ref> and [[Lake Ayakkum]] ({{zh|c=阿牙克库木湖|p=Āyákèkùmù hú}}; 37°30′N,89°30′E; elevation 3,876 m).<ref name=LiBosheng/><ref>Or 3,870 m, according to [http://www.hudong.com/wiki/阿牙克库木湖 阿牙克库木湖] (Ayakkum Lake) on Hudong.com</ref> These lakes are two of the few noticeable bodies of water in this extremely arid area; the area around them is officially protected as the '''[[Altun Shan Nature Reserve]]'''.<ref name=LiBosheng>{{citation
The two main lakes in this basin are the saline [[Lake Aqqikkol]] (also Ajig Kum Kul,<ref>Holdich, Sir Thomas (2006); p. 228</ref> Achak-kum; {{zh|c=阿其克库勒湖|p= Āqíkèkùlè Hú}}; 37°05′N,88°25′E, {{convert|4250|m|ft}} elevation)<ref>www.baidu.com (2013)</ref> and [[Lake Ayakkum]] ({{zh|c=阿牙克库木湖|p=Āyákèkùmù hú}}; 37°30′N,89°30′E; elevation {{convert|3876|m|ft}}).<ref name=LiBosheng/> These lakes are two of the few noticeable bodies of water in this extremely arid area; the area around them is officially protected as the '''[[Altun Shan Nature Reserve]]'''.<ref name=LiBosheng>Li, Bosheng (2000); pp. 230-231</ref>
|contribution=Chapter 11, Nature Conservation
|first=Bosheng |last=Li
|editor-first=Du |editor-last=Zheng|editor2-first= Qingsong |editor2-last=Zhang|editor3-first= Shaohong |editor3-last=Wu
|publisher=Springer |year=2000
|isbn=0-7923-6688-3
|title=Mountain geoecology and sustainable development of the Tibetan Plateau
|series=Volume 57 of GeoJournal library
|url= http://books.google.com/books?id=DuwwoxDxCYAC&pg=PA230
|pages=230–231
}}</ref>


Farther east, in northwestern [[Qinghai]], the much larger [[Qaidam Basin]] starts between the Altyn-Tagh and the Kunlun and extends almost to the east side of the plateau<!-- wich? -->; the Altyn-Tagh separates the west side of this basin from the [[Kumtagh Desert]].
Farther east, in northwestern [[Qinghai]], the much larger [[Qaidam Basin]] starts between the Altyn-Tagh and the Kunlun and extends almost to the east side of the plateau<!-- wich? -->; the Altyn-Tagh separates the west side of this basin from the [[Kumtagh Desert]].
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==Major Peaks==
==Major Peaks==
The six highest peaks are [[Ak Tag]] (6748 m), [[Sulamutag Feng]] (6245 m), [[Yusupu Aleketag Shan]] (6065 m), Altun Shan (5830 m), [[Muzluktag]] (5766 m) and [[Kogantag]] (4800 m).<ref name="Peakbagger">{{cite web|url=http://www.peakbagger.com/range.aspx?rid=471|title=Altun Shan|last=Peakbagger.com|date=1 November 2004|accessdate=17 July 2010}}</ref><ref name="Peaklist">{{cite web|url=http://www.peaklist.org/WWlists/ultras/china2.html|title=Sinkiang - Xinjiang 53 Mountain Summits with Prominence of 1,500 meters or greater|last=Peaklist|accessdate=24 July 2010| archiveurl= http://web.archive.org/web/20100823115605/http://www.peaklist.org/WWlists/ultras/china2.html| archivedate= 23 August 2010 <!--DASHBot-->| deadurl= no}}</ref>
The six highest peaks are [[Ak Tag]] (6748 m), [[Sulamutag Feng]] (6245 m), [[Yusupu Aleketag Shan]] (6065 m), Altun Shan (5830 m), [[Muzluktag]] (5766 m) and [[Kogantag]] (4800 m).<ref name="Peakbagger">www.peakbagger.com (2004)</ref><ref name="Peaklist">de Ferranti, Jonathan; Jurgalski, Eberhard; Maizlish, Aaron (2010)</ref>


==Economic development==
==Economic development==
[[China National Highway 315]] crosses the Altyn-Tagh on its way between Qinghai and Xinjiang.
[[China National Highway 315]] crosses the Altyn-Tagh on its way between Qinghai and Xinjiang.


As of the late 2013, preliminary planning is conducted for the [[Kurla]]-Golmud Railway, which, if constructed, will cross the Altyn-Tagh as well.<ref>[http://news.huochepiao.com/2013-9/201393016361164.htm 库尔勒—格尔木铁路项目预可研报告获批] (Kurla-Golmud Railway project preliminary feasibility study report approved), 中华铁道网, 2013-09-30</ref>
As of the late 2013, preliminary planning is conducted for the [[Kurla]]-Golmud Railway, which, if constructed, will cross the Altyn-Tagh as well.


==Notes==
==Notes==
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==References==
==References==
* {{cite web | url = http://baike.baidu.com/view/283650.htm | title = 阿其克库勒湖(A lake whose Ke Kule) | author = www.Baidu.com | year = 2013 | accessdate = 11/06/2013 }}
* {{cite web | url = http://baike.baidu.com/view/283650.htm | title = 阿其克库勒湖(A lake whose Ke Kule) | author = www.Baidu.com | year = 2013 | accessdate = 11/06/2013 }}
* {{cite book | chapter = Nature Conservation | first = Bosheng | last = Li | editor1-last = Du Zheng | editor1-first = Qingsong Zhang | editor2-first = Shaohong |editor2-last = Wu | publisher = Springer Science + Business Media Dordrecht | year = 2000 | isbn = 978-94-010-3800-3 | title = Mountain Geoecology and Sustainable Development of the Tibetan Plateau | series = GeoJournal library |volume = 57 | url = http://books.google.com/books?id=DuwwoxDxCYAC&pg=PA230 |doi = 10.1007/978-94-010-0965-2}}
* {{cite encyclopedia | editor-first = Dale H. | editor-last = Hoiberg | encyclopedia = Encyclopedia Britannica | title = A-erh-chin Mountains | edition = 15th | year = 2010 | publisher = Encyclopedia Britannica, Inc. | volume = I: A-Ak - Bayes | location = Chicago, IL | isbn = 978-1-59339-837-8 | pages = 1}}
* {{cite encyclopedia | editor-first = Dale H. | editor-last = Hoiberg | encyclopedia = Encyclopedia Britannica | title = A-erh-chin Mountains | edition = 15th | year = 2010 | publisher = Encyclopedia Britannica, Inc. | volume = I: A-Ak - Bayes | location = Chicago, IL | isbn = 978-1-59339-837-8 | pages = 1}}
* {{cite book | first = Sir Thomas | last = Holdich | publisher = Adamant Media Corporation | origyear=1906 | year = 2006 |title = Tibet, the Mysterious | page=288
* {{cite book | first = Sir Thomas | last = Holdich | publisher = Adamant Media Corporation | origyear=1906 | year = 2006 |title = Tibet, the Mysterious | page=288
| url = http://books.google.com/books?id=Wz8TAAAAYAAJ&pg=PA288 | isbn = 1-4212-8483-9 | series = Elibron Classic Series | editor-first = J. Scott | editor-last = Keltie }}
| url = http://books.google.com/books?id=Wz8TAAAAYAAJ&pg=PA288 | isbn = 1-4212-8483-9 | series = Elibron Classic Series | editor-first = J. Scott | editor-last = Keltie }}
* {{cite web | url = http://www.hudong.com/wiki/阿牙克库木湖 阿牙克库木湖 | title = Ayakkum Lake | publisher = www.baike.com | author = www.baike.com year = 2013 }}
* {{cite journal | title = Cenozoic Tectonic Development of the Qaidam Basin in the Northeastern Tibetan Plateau | first1 = Qing-Ren | last1 = Meng | first2 = Xiang | last2 = Fang | editor-first = B. C. | editor-last = Burchfield | editor2-first = Erchie | editor2-last = Wang | publisher = Geological Society of America | year = 2008 | doi = 10.1130/2008.2444(01) | journal = Special Paper - Geological Society Of America | volume = 444 | url = http://books.google.com/books?id=BligM888ki0C&pg=PA1 | pages = 1–24}}
* {{cite journal | title = Cenozoic Tectonic Development of the Qaidam Basin in the Northeastern Tibetan Plateau | first1 = Qing-Ren | last1 = Meng | first2 = Xiang | last2 = Fang | editor-first = B. C. | editor-last = Burchfield | editor2-first = Erchie | editor2-last = Wang | publisher = Geological Society of America | year = 2008 | doi = 10.1130/2008.2444(01) | journal = Special Paper - Geological Society Of America | volume = 444 | url = http://books.google.com/books?id=BligM888ki0C&pg=PA1 | pages = 1–24}}

* {{cite book | first = Mianping | last = Zheng | publisher = Springer | year=1997 | isbn = 978-0792340980 | title = An introduction to saline lakes on the Qinghai-Tibet plateau | series = Monographiae Biologicae |volume = 76 | url = http://books.google.com/books?id=NvD-RMX58cIC&pg=PA229 }}
* {{cite book | first = Mianping | last = Zheng | publisher = Springer | year=1997 | isbn = 978-0792340980 | title = An introduction to saline lakes on the Qinghai-Tibet plateau | series = Monographiae Biologicae |volume = 76 | url = http://books.google.com/books?id=NvD-RMX58cIC&pg=PA229 }}
* {{cite web | url = http://www.peakbagger.com/range.aspx?rid=471 | title = Altun Shan | author = www.peakbagger.com | year = 2004 | accessdate = 17 July 2010 }}
* {{cite web | url = http://www.peaklist.org/WWlists/ultras/china2.html | first1 = Jonathan | last1 = de Ferranti | first2 = Eberhard | last2 = Jurgalski | first3 = Aaron | last3 = Maizlish | title = Sinkiang - Xinjiang | publisher = www.peaklist.com | accessdate = 24 July 2010 | archiveurl = http://web.archive.org/web/20100823115605/http://www.peaklist.org/WWlists/ultras/china2.html | archivedate = 23 August 2010 <!--DASHBot-->| deadurl = no | year = 2006 }}


==Further reading==
==Further reading==

Revision as of 09:44, 7 November 2013

39°00′N 92°00′E / 39.000°N 92.000°E / 39.000; 92.000

Eastern part of Altun Shan at bottom of elevation map
For neighborhoods in Turkish cities, see Altındağ, İzmir and Altındağ, Ankara

Altyn-Tagh, (Astyn-Tagh, Altun Mountains, Pinyin: Altun Shan, A-erh-chin, Wade–Giles:A-erh-chin shan, Aerjin Shan, (Chinese: 阿尔金山))[1] is a part of the range south of Lop Nor), and is a mountain range in northwestern China that separates the eastern Tarim Basin from the Tibetan Plateau. The western third is in Xinjiang while the eastern part forms the border between Qinghai to the south and Xinjiang and Gansu to the north.

Altun Shan is also the name of a 5,830 metres (19,130 ft) mountain near the eastern end of the range.

Etymology

Altyn Tag means Gold Mountain in Turkic, and Shan is Chinese for mountain.

Geography

A series of mountain ranges run along the northern edge of the Tibetan Plateau. In the west are the Kunlun Mountains. About half way across the Tarim basin, where the mountains begin to orient somewhat to the north, the border range becomes the Altyn-Tagh, while the Kunluns continue directly east, forming a "V".[nb 1] Inside the "V" are a number of endorheic basins. The eastern end of the Altyn-Shan is near the Dangjin Pass on the Dunhuang-Golmud road in far western Gansu. East of the Altyn-Tagh the border range rises to the Qilian Mountains. The range separates the Tarim Basin, to the north, and Lake Ayakkum, to the south. The range can be divided into three portions. The southwest portion borders the Kunlun Mountains, is very rugged, with peaks reaching more than 6,100 metres (20,000 ft) and many perrenial snow fields. The central portion is lower in elevation, around 4,000 metres (13,000 ft), and the eastern portion. The eastern portion is higher in elevation, about 5,000 metres (16,000 ft) and consists of a group of smaller ranges oriented in a south-east to north-west trend.[1]

Along the northern side of the mountains ran the main Silk road trade route from China proper to the Tarim Basin and westward. The Altun-Tagh and Qilians were sometimes called the Nan Shan ('south mountains') because they were south of the main route. Near the west end of the Altun-Shan the Gansu or Hexi corridor ends and the silk road splits. One branch follows the Altun-Tagh along the south side of the Tarim Basin while the other follows the north side.

The southwestern part of the Altyn-Tagh range reaches snowy peaks of up to 6,295 metres (20,653 ft), although it descends to an average of 4,000 metres (13,000 ft) in the narrow middle and eventually rises up to average 5,000 metres (16,000 ft) as it meets the Nan Shan.

There are a dearth of rivers and streams in these mountains, due to the aridity of the region. The western portion has some small streams that either head north into the dessert or south into Lake Ayakkum. The remainder of the range is lacking in rivers.[1]

Intermontane endorheic basins

Inside the "V" shaped area between the Altyn-Tagh and the main Kunlun range (which in this area is called Arka-Tagh) a number of endorheic basins are located.

Within southeastern Xinjiang, the main of these basins is the Kumkol Basin (Chinese: 库木库里盆地; pinyin: Kùmùkùlǐ Péndì)[nb 2]

The two main lakes in this basin are the saline Lake Aqqikkol (also Ajig Kum Kul,[5] Achak-kum; Chinese: 阿其克库勒湖; pinyin: Āqíkèkùlè Hú; 37°05′N,88°25′E, 4,250 metres (13,940 ft) elevation)[6] and Lake Ayakkum (Chinese: 阿牙克库木湖; pinyin: Āyákèkùmù hú; 37°30′N,89°30′E; elevation 3,876 metres (12,717 ft)).[7] These lakes are two of the few noticeable bodies of water in this extremely arid area; the area around them is officially protected as the Altun Shan Nature Reserve.[7]

Farther east, in northwestern Qinghai, the much larger Qaidam Basin starts between the Altyn-Tagh and the Kunlun and extends almost to the east side of the plateau; the Altyn-Tagh separates the west side of this basin from the Kumtagh Desert.

Major Peaks

The six highest peaks are Ak Tag (6748 m), Sulamutag Feng (6245 m), Yusupu Aleketag Shan (6065 m), Altun Shan (5830 m), Muzluktag (5766 m) and Kogantag (4800 m).[8][9]

Economic development

China National Highway 315 crosses the Altyn-Tagh on its way between Qinghai and Xinjiang.

As of the late 2013, preliminary planning is conducted for the Kurla-Golmud Railway, which, if constructed, will cross the Altyn-Tagh as well.

Notes

  1. ^ See e.g. the map in Fig. 1 in Meng & Fang's Cenozoic tectonic development of the Qaidam Basin in the northeastern Tibetan Plateau[2]
  2. ^ The Chinese-based spelling (pinyin) for this place name, "Kumukuli Basin" is often used in English. When trying to produce a Turkic-like spelling for this name, authors occasionally transcribe it as "Kumukol Basin", as in the map in Fig. 2 in Meng & Fang's Cenozoic tectonic development of the Qaidam Basin in the northeastern Tibetan Plateau,[3] but more often as "Kumkol",[4] or "Kumkuli".

Footnotes

  1. ^ a b c Hoiberg, Dale H. (2010)
  2. ^ Meng, Qing-Ren; Fang, Xiang (2008) p. 2
  3. ^ Meng, Qing-Ren; Fang, Xiang (2008) p. 3
  4. ^ Zheng, Mianping (1997) p. 229
  5. ^ Holdich, Sir Thomas (2006); p. 228
  6. ^ www.baidu.com (2013)
  7. ^ a b Li, Bosheng (2000); pp. 230-231
  8. ^ www.peakbagger.com (2004)
  9. ^ de Ferranti, Jonathan; Jurgalski, Eberhard; Maizlish, Aaron (2010)

References

  • www.Baidu.com (2013). "阿其克库勒湖(A lake whose Ke Kule)". Retrieved 11/06/2013. {{cite web}}: Check date values in: |accessdate= (help)
  • Li, Bosheng (2000). "Nature Conservation". In Du Zheng, Qingsong Zhang; Wu, Shaohong (eds.). Mountain Geoecology and Sustainable Development of the Tibetan Plateau. GeoJournal library. Vol. 57. Springer Science + Business Media Dordrecht. doi:10.1007/978-94-010-0965-2. ISBN 978-94-010-3800-3.
  • Hoiberg, Dale H., ed. (2010). "A-erh-chin Mountains". Encyclopedia Britannica. Vol. I: A-Ak - Bayes (15th ed.). Chicago, IL: Encyclopedia Britannica, Inc. p. 1. ISBN 978-1-59339-837-8.
  • Holdich, Sir Thomas (2006) [1906]. Keltie, J. Scott (ed.). Tibet, the Mysterious. Elibron Classic Series. Adamant Media Corporation. p. 288. ISBN 1-4212-8483-9.
  • www.baike.com year = 2013. 阿牙克库木湖 "Ayakkum Lake". www.baike.com. {{cite web}}: Check |url= value (help); Missing pipe in: |author= (help)CS1 maint: numeric names: authors list (link)
  • Meng, Qing-Ren; Fang, Xiang (2008). Burchfield, B. C.; Wang, Erchie (eds.). "Cenozoic Tectonic Development of the Qaidam Basin in the Northeastern Tibetan Plateau". Special Paper - Geological Society Of America. 444. Geological Society of America: 1–24. doi:10.1130/2008.2444(01).
  • Zheng, Mianping (1997). An introduction to saline lakes on the Qinghai-Tibet plateau. Monographiae Biologicae. Vol. 76. Springer. ISBN 978-0792340980.
  • www.peakbagger.com (2004). "Altun Shan". Retrieved 17 July 2010.
  • de Ferranti, Jonathan; Jurgalski, Eberhard; Maizlish, Aaron (2006). "Sinkiang - Xinjiang". www.peaklist.com. Archived from the original on 23 August 2010. Retrieved 24 July 2010. {{cite web}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

Further reading

  • National Geographic Atlas of China. Washington, DC: National Geographic. 2009. ISBN 978-1426203275.

External links

Public Domain This article incorporates text from a publication now in the public domainChisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press. {{cite encyclopedia}}: Missing or empty |title= (help)