The Kregnes moraine in Gauldalen, west‐central Norway: anatomy of a Younger Dryas proglacial delta in a palaeofjord basin*

The Kregnes “moraine” ridge in Gauldalen, a north‐trending valley south of Trondheim, is a Gilbert‐type delta formed at a Younger Dryas glacier terminus. The gravelly delta consists of a north‐dipping foreset, 150 m thick, comprised of turbidites, debrisflow beds and debrisfall deposits. The bottoms...

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Bibliographic Details
Published in:Boreas
Main Authors: NEMEC, W., LφNNE, IDA, BLIKRA, LARS H.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1999
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1999.tb00234.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1999.tb00234.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1999.tb00234.x