Glaciation's topographic control on Holocene erosion at the eastern edge of the Alps

What is the influence of glacial processes in driving erosion and uplift across the European Alps? It has largely been argued that repeated erosion and glaciation sustain isostatic uplift and topography in a decaying orogen. But some parts of the Alps may still be actively uplifting via deep lit...

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Bibliographic Details
Main Authors: J. L. Dixon, F. von Blanckenburg, K. Stüwe, M. Christl
Format: Article
Language:English
Published: Copernicus Publications 2016-12-01
Series:Earth Surface Dynamics
Online Access:https://www.earth-surf-dynam.net/4/895/2016/esurf-4-895-2016.pdf