Terminal zone glacial sediment transfer at a temperate overdeepened glacier system

Continuity of sediment transfer through glacial systems is essential to maintain subglacial bedrock erosion, yet transfer at temperate glaciers with overdeepened beds, where subglacial fluvial sediment transport should be greatly limited by adverse slopes, remains poorly understood. Complex multiple...

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Bibliographic Details
Main Authors: Darrel A. Swift, Simon J. Cook, David Graham, Nicholas G. Midgley, A.E. Fallick, R. Storrar, R. Toubes Rodrigo, D.J.A. Evans
Format: Default Article
Published: 2017
Subjects:
Other earth sciences not elsewhere classified
Present
Quaternary
Glaciation
Glaciology
Europe
Geomorphology
Glacial
Sediment transport
Glacial erosion
Glacial hydrology
Earth Sciences not elsewhere classified
Online Access:https://hdl.handle.net/2134/27782
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https://hdl.handle.net/2134/27782

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