Denudation of the continental shelf between Britain and France at the glacial-interglacial timescale

The erosional morphology preserved at the sea bed in the eastern English Channel dominantly records denudation of the continental shelf by fluvial processes over multiple glacial-interglacial sea-level cycles rather than by catastrophic flooding through the Straits of Dover during the mid-Quaternary...

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Bibliographic Details
Published in:Geomorphology
Main Authors: Mellett, CL, Hodgson, DM, Plater, AJ, Mauz, B, Selby, I, Lang, A
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2013
Subjects:
Online Access:https://eprints.whiterose.ac.uk/77090/
https://eprints.whiterose.ac.uk/77090/1/mellett_etal_2013_geomorph_final.pdf
https://doi.org/10.1016/j.geomorph.2013.03.030