Evolution of Glacial Lake Cochrane During the Last Glacial Termination, Central Chilean Patagonia (similar to 47 degrees 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 fluctuatio FONDECYT REGULAR Proyectos de Investigación...

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Bibliographic Details
Published in:Frontiers in Earth Science
Main Authors: Vásquez, Alicia, Flores-Aqueveque, Valentina, Sagredo, Esteban, Hevia-Esquivel, Rodrigo Ignacio, Villa-Martínez, Rodrigo Patricio, Moreno, Patricio I, Antinao, José L
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Geosciences
Multidisciplinary
Glacial Lake
Patagonia
Ice Sheet
Online Access:https://hdl.handle.net/10533/72882
https://doi.org/10.3389/feart.2022.817775
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Summary: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 fluctuatio FONDECYT REGULAR Proyectos de Investigación wos 10

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