Chuya Steppe: Difference between revisions
Appearance
Content deleted Content added
m r2.7.1) (Robot: Adding fr:Steppe de la Tchouïa |
|||
Line 21: | Line 21: | ||
[[Category:Temperate grasslands, savannas, and shrublands]] |
[[Category:Temperate grasslands, savannas, and shrublands]] |
||
[[fr:Steppe de la Tchouïa]] |
|||
[[ka:ჩუიის სტეპი]] |
[[ka:ჩუიის სტეპი]] |
||
[[nl:Tsjoejasteppe]] |
[[nl:Tsjoejasteppe]] |
Revision as of 00:52, 4 July 2012
The Chuya Steppe in the Siberian Altai Mountains is a depression formed by tectonic movement of major faults in the Earths crust. The name 'Chuya Steppe' comes from the large river which runs through the steppe, the Chuya River.
Major Settlements
Kosh-Agach is a major village in the north of the steppe. Other large settlements include Chaganuzun and Beltir.
Geology
The Chuya Steppe is filled with Cenozoic sediments, derived from the surrounding mountains of the Chuya Range-Chuya Alps.
Seismicity
In September 2003, a major earthquake occurred in the Chuya Steppe which caused regional devastation. Major movement considered to have occurred on the Chuya thrust fault caused this earthquake, of magnitude 7.3. The USGS estimates that this caused $10.6 million damage.