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More model informationA cliif of the Volga river, where internal structure of what is known as Baer Knolls, is nicely exposed. The Baer Knolls are elongated hills, which are distributed over a large part of the Caspian Lowland. They were formed about 10 000-15 000 years ago and were extensively studied over last 200 years, but their geological origin is still enigmatic.
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