Evolution of Glacial Lake Cochrane During the Last Glacial Termination, Central Chilean Patagonia (∼47°S)

Large ice-dammed lakes developed along the eastern margin of the Patagonian Ice Sheet (PIS) during the Last Glacial Termination (T1). Their spatial/temporal evolution, however, remains poorly constrained despite their importance for deciphering fluctuations of the shrinking PIS, isostatic adjustment...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Alicia Vásquez, Valentina Flores-Aqueveque, Esteban Sagredo, Rodrigo Hevia, Rodrigo Villa-Martínez, Patricio I. Moreno, Jose L. Antinao
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
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Online Access:https://doi.org/10.3389/feart.2022.817775
https://doaj.org/article/bce232ce214d420ca0462541383b5ee3