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Degradation of unconsolidated Quaternary landforms in the western North America

✍ Scribed by Jaakko Putkonen; Michael O'Neal


Book ID
116510661
Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
891 KB
Volume
75
Category
Article
ISSN
0169-555X

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## Abstract The West Siberian Plain was formed by marine deposits that extended from the Mediterranean basin to the arctic. Tectonic action later produced a striking series of long straight NE–SW grabens in the southern part of the plain. Pleistocene advance of the Kara ice sheet onto the continent