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

• Main Authors: Alicia Vásquez (11996957), Valentina Flores-Aqueveque (11996960), Esteban Sagredo (8670819), Rodrigo Hevia (11996963), Rodrigo Villa-Martínez (11996966), Patricio I. Moreno (11996969), Jose L. Antinao (11996972)
• 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

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...