A comparison of glacial and paraglacial denudation responses to rapid glacial retreat

Glacier thinning and retreat drives initial acceleration of glacier sliding and erosion, de-buttressing of steep valley walls, and destabilization of ice-marginal deposits and bedrock, which can lead to massive rock avalanching and accelerated incision of tributary watersheds. A compelling example o...

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Bibliographic Details
Main Authors: Haley B. Williams, Michele N. Koppes
Format: Article
Language:English
Published: Cambridge University Press 2019-12-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305520000014/type/journal_article