A Glacial Landform Assemblage from an Inter-ice Stream Setting in the Eastern Amundsen Sea Embayment, West Antarctica

Large ice streams that drain the West Antarctic Ice Sheet (WAIS) into the Amundsen Sea Embayment (ASE) are currently thinning, accelerating and retreating rapidly (e.g. Rignot et al. 2014). These ice streams are assumed to have reached the continental shelf edge during the Last Glacial Maximum (LGM;...

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Bibliographic Details
Published in:Geological Society, London, Memoirs
Main Authors: Klages, J. P., Kuhn, G., Hillenbrand, C.-D., Graham, A. G. C., Smith, J. A., Larter, R. D., Gohl, K.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2016
Subjects:
Online Access:https://digitalcommons.usf.edu/msc_facpub/1567
https://doi.org/10.1144/M46.147