Modelling the diversion of erratic boulders by the Valais Glacier during the last glacial maximum

In this study, a modelling approach was used to investigate the cause of the diversion of erratic boulders from Mont Blanc and southern Valais by the Valais Glacier to the Solothurn lobe during the Last Glacial Maximum (LGM). Using the Parallel Ice Sheet Model, we simulated the ice flow field during...

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Bibliographic Details
Main Authors: Jouvet, Guillaume, Seguinot, Julien, Ivy-Ochs, Susan, Funk, Martin
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2017
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/190439
https://doi.org/10.3929/ethz-b-000190439