Ice-stream flow switching during deglaciation of the southwestern Barents Sea.

Ice streams dominate the discharge of continental ice sheets. Recent observations and reconstructions have revealed that large-scale reorganizations in their flow trajectory (flow switching) can occur over relatively short time scales. However, the underlying causes of such behavior, and the extent...

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Bibliographic Details
Published in:Geological Society of America Bulletin
Main Authors: Winsborrow, M.C.M., Stokes, C.R., Andreassen, K.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2012
Subjects:
Online Access:http://dro.dur.ac.uk/11094/
https://doi.org/10.1130/B30416.1