## 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 NEβSW grabens in the southern part of the plain. Pleistocene advance of the Kara ice sheet onto the continent
β¦ LIBER β¦
Quaternary landscape change and modern process in western North America
β Scribed by Jeffrey S. Munroe; Benjamin J.C. Laabs; Eric C. Carson
- Book ID
- 116510660
- Publisher
- Elsevier Science
- Year
- 2006
- Tongue
- English
- Weight
- 63 KB
- Volume
- 75
- Category
- Article
- ISSN
- 0169-555X
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