Marginal formation of De Geer moraines and their implications to the dynamics of grounding-line recession

De Geer moraine ridges occur in abundance in the coastal zone of northern Sweden, preferentially in areas with proglacial water depths in excess of 150 m at deglaciation. From detailed sedimentological and structural investigations in machine-dug trenches across De Geer ridges it is concluded that t...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Lindén, Mattias, Möller, Per
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2005
Subjects:
Online Access:https://lup.lub.lu.se/record/249906
https://doi.org/10.1002/jqs.902