The Wusun Mountains[1] or Ketmen Mountains are a small range in the central part of the Tianshan Mountains. They lie north of the Tekes River valley and south of the main Ili River valley in southeastern Kazakhstan and in western Xinjiang Province, China. The highest point is Baishi Peak (白石峰), about 3,475 meters (11,400 ft) above sea level.
Wusun Mountains | |||||||
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![]() A 1997 photograph of the Tianshan from space, its Wusun part lying in the top right between the wide Tekes and Ili valleys | |||||||
Traditional Chinese | 烏孫山(脉) | ||||||
Simplified Chinese | 乌孙山(脉) | ||||||
Literal meaning | Wusun Mountain (Range) | ||||||
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![](http://upload.wikimedia.org/wikipedia/commons/thumb/9/93/A-k%60o-su_NK-44_%281950%29_-_panoramio.jpg/250px-A-k%60o-su_NK-44_%281950%29_-_panoramio.jpg)
Names
editWūsūn is the pinyin form of the Chinese name written 烏孫 in traditional characters and 乌孙 in simplified ones, taken from the ancient Wusun people. It is sometimes distinguished as particularly the Chinese part of the range, the Kazakh area being the Ketmen Ridge.[2]
The mountains have also been known as the Karatau (Russian: Каратау), Qaratau (Қаратау, "Black Mountain"), Temirlik (Kazakh: Темирлик, "Iron-Bearing" or "Producing"), and Nánshān (南山, "South" or "Southern Mountains").[3]
See also
editReferences
editCitations
edit- ^ Su & al. (2021).
- ^ Mikolaichuk & al. (2023).
- ^ "Ili", Encyclopaedia Britannica, vol. XII (9th ed.), 1881.
Bibliography
edit- Mikolaichuk, A.; et al. (2023), "Correlation of Geological Complexes of the Khan-Tengri Mountain Massif in Border Regions of the Kyrgyz, Kazakh, and Chinese Tianshan", Regional'naya Geologia Региональная Геология [Regional Geology] (in Russian), doi:10.26516/2541-9641.2023.4.7.
- Su Wenbo; et al. (November 2021), "Carboniferous Back-Arc Extension in the Southern Yili-Central Tianshan Block and Its Significance to the Formation of the Kazakhstan Orocline: Insites from the Wusun Mountain Volcanic Belt", International Journal of Earth Sciences, vol. 111, Berlin: Geologische Vereinigung e.V., doi:10.1007/s00531-021-02111-y.