Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Turpan Depression
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Geology and relief== The Turpan Basin is a fault-bounded trough located in the eastern part of the [[Tian Shan]]. It covers an area of {{convert|50000|km2}}. The surrounding mountain ranges are: the central Tian Shan in the west, the [[Bogda Shan]] in the north-west, the Haerlike Shan in the north-west, and the Jueluotage Shan in the south. Beyond the surrounding mountain ranges lie the [[Dzungaria|Junggar Basin]] in the north and the [[Tarim Basin]] in the south. Some geographers also use the term Turpan-Hami Basin, which is understood as including the Turpan Depression along with the [[Hami Depression]] (located to the east of the Turpan Depression, and to the southwest of the city of [[Hami City|Hami]]) and the Liaodong Uplift separating the two depressions. A source using this terminology gave the area of the Turpan Depression proper as {{convert|28600|km2|abbr=on}}, that of the Hami Depression as {{convert|19300|km2|abbr=on}}, and for the entire Turpan-Hami Basin, as {{convert|48000|km2|abbr=on}}.<ref name=uranium>{{citation |first=Franz J.|last=Dahlkamp |isbn=978-3-540-78557-6 |title=Uranium Deposits of the World: Asia |publisher= Springer |url= https://books.google.com/books?id=ShzwRGs5mDYC&pg=PA40 |pages=40β41 |date=2009-09-16 }}</ref> [[Image:Turpan-flaming-mountains-camellos-d01.jpg|thumb|250px|Basin scene near [[Flaming Mountains]]]] The Turpan Basin formed in a [[shear zone]] during the [[Lopingian|Late Permian]] due to motion between the [[East European craton|East European]] and the [[Angaran craton]]. It was subsequently deformed by the collision of the [[Indian Plate]] and [[Eurasian Plate]] in the [[Cenozoic]]. In the latter deformation, a thrust fault belt running from east to west, the [[Flaming Mountains]], was formed in the center of the basin. The Flaming Mountains are {{convert|98|km|abbr=on}} long and {{convert|9|km|abbr=on}} wide; the highest peak reaches an elevation of {{convert|831.7|m|abbr=on}} above sea level. The Turfan volcano is located near Turpan. Also in the center of the basin lies the [[Ayding Lake]] (Moonlight Lake) which has an elevation of {{convert|154.5|m|abbr=on}} below sea level, the [[List of elevation extremes by country|sixth lowest exposed elevation on the Earth's land surface]]. It is the lowest surface point in China. The Shihongtan [[uranium]] ore deposit is located at the southwestern margin of the Turpan Depression, some {{convert|35|km|abbr=on}} south-southwest from Turpan City.<ref name=uranium/>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)