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Science (New York, N.Y.)
|March 18, 1966
PubMed
概括

德鲁姆林是从冰川下方的岩石粘土中形成的流线式山丘. 粘土颗粒的行为会产生阻碍物,这些阻碍物会重定向冰川流动,从而塑造出这些独特的地形.

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