Abstract
Recent research on the Upper Pleistocene loessic formations of northwestern and central Europe have shown that in both regions the main loess cover has been deposited between ±25 000 and ±20 000 B.P., essentially before the last maximum extend of the Scandinavian ice sheet. Nevertheless, in some areas of central Europe the loessic sedimentation was active up to the end of the Weichselian.

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