Ice-stream demise dynamically conditioned by trough shape and bed strength

Tom Bradwell1,2, David Small3, Derek Fabel4

  • 1Biological and Environmental Sciences, University of Stirling, Stirling FK9 4LA, UK.

Science Advances
|May 7, 2019
PubMed
Summary

Glacial ice stream retreat was significantly influenced by bed strength and trough shape, not just external factors. A transition from weak to strong beds around 18,500 years ago triggered rapid ice-stream demise.

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