Glacial geomorphology of the former Patagonian Ice Sheet (44–46 °S)

• Main Authors: Cooper, Emma-Louise, Thorndycraft, Varyl R., Davies, Bethan J., Palmer, Adrian P., García, Juan-Luis
• Format: Other Non-Article Part of Journal/Newspaper
• Language: unknown
• Published: Taylor & Francis 2021
• Subjects: 59999 Environmental Sciences not elsewhere classified; FOS Earth and related environmental sciences; Ecology; FOS Biological sciences; 20199 Astronomical and Space Sciences not elsewhere classified; FOS Physical sciences; 69999 Biological Sciences not elsewhere classified; Computational Biology; Caceres; El Toqui; Fontana; Patagonia; Ice Sheet
• Online Access: https://dx.doi.org/10.6084/m9.figshare.17157906.v1; https://tandf.figshare.com/articles/journal_contribution/Glacial_geomorphology_of_the_former_Patagonian_Ice_Sheet_44_46_S_/17157906/1

We map the glacial geomorphology of the former Patagonian Ice Sheet between 44°S and 46°S. Building on previous work, our map covers a ∼50,000 km 2 region of west-central Patagonia. The study area includes the eastward-flowing Río Pico, Río Caceres, Río Cisnes, Lago Plata-Fontana, El Toqui, Lago Coyt/Río Ñirehuao, Simpson/Paso Coyhaique, and Balmaceda palaeo-outlet glaciers, adjacent valleys, and the Andean Cordillera. The inventory contains >70,000 individual landforms mapped from remotely-sensed imagery and field surveys. Mapping was classified into ice-marginal (e.g. moraine ridges, trimlines), subglacial (e.g. glacial lineations, flutes), glaciolacustrine (e.g. palaeolake shorelines, perched deltas), glaciofluvial (e.g. proglacial outwash plains, meltwater channels), and non-glacial (e.g. palaeochannels, landslides or slumps) landform groups. The new map will inform future interpretations of regional glacier dynamics, and the development of robust geochronological datasets that test the timing of glaciation and deglaciation.