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

Abstract 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 conclud...

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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: Wiley 2005
Subjects:
Online Access:http://dx.doi.org/10.1002/jqs.902
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.902
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.902