Comparison of overdeepened structures in formerly glaciated areas of the northern Alpine foreland and northern central Europe

<p>Overdeepened structures occur in formerly and presently glaciated regions around the earth and are usually referred to as overdeepenings or tunnel valleys. The existence of such troughs has been known for more than a century, and they have been attributed to similar formation processes wher...

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Bibliographic Details
Main Authors: L. Gegg, F. Preusser
Format: Article
Language:deu
Published: Copernicus Publications 2023-01-01
Series:Eiszeitalter und Gegenwart
Online Access:https://egqsj.copernicus.org/articles/72/23/2023/egqsj-72-23-2023.pdf