DataSheet1_Evolution of Glacial Lake Cochrane During the Last Glacial Termination, Central Chilean Patagonia (∼47°S).docx

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
Main Authors: Alicia Vásquez, Valentina Flores-Aqueveque, Esteban Sagredo, Rodrigo Hevia, Rodrigo Villa-Martínez, Patricio I. Moreno, Jose L. Antinao
Format: Dataset
Language:unknown
Published: 2022
Subjects:
Solid Earth Sciences
Climate Science
Atmospheric Sciences not elsewhere classified
Exploration Geochemistry
Inorganic Geochemistry
Isotope Geochemistry
Organic Geochemistry
Geochemistry not elsewhere classified
Igneous and Metamorphic Petrology
Ore Deposit Petrology
Palaeontology (incl. Palynology)
Structural Geology
Tectonics
Volcanology
Geology not elsewhere classified
Seismology and Seismic Exploration
Glaciology
Hydrogeology
Natural Hazards
Quaternary Environments
Earth Sciences not elsewhere classified
Evolutionary Impacts of Climate Change
glacial lake cochrane
last glacial termination
isostatic rebound
central patagonia
patagonian ice sheet
Patagonia
Pacific
Glacial Lake
Ice Sheet
Online Access:https://doi.org/10.3389/feart.2022.817775.s001
https://figshare.com/articles/dataset/DataSheet1_Evolution_of_Glacial_Lake_Cochrane_During_the_Last_Glacial_Termination_Central_Chilean_Patagonia_47_S_docx/19030040

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