Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)

We present the first extensive high-resolution glacial geomorphic map west of the Andean Cordillera in southernmost Chile (52.8–53.1°S, 73.0–73.9°W). The map extends over 1565 km2 and is based on high-resolution satellite images and aerial photographs. At selected locations, the remotely mapped geom...

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Published in:Journal of Maps
Main Author: Smedley, Rachel
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2023
Subjects:
Online Access:http://livrepository.liverpool.ac.uk/3170138/
https://doi.org/10.1080/17445647.2022.2153091
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spelling ftunivliverpool:oai:livrepository.liverpool.ac.uk:3170138 2023-08-27T04:10:02+02:00 Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W) Smedley, Rachel 2023-05-03 http://livrepository.liverpool.ac.uk/3170138/ https://doi.org/10.1080/17445647.2022.2153091 en eng Taylor & Francis Group Smedley, Rachel orcid:0000-0001-7773-5193 (2023) Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W). Journal of Maps, 19 (1). pp. 1-14. Article NonPeerReviewed 2023 ftunivliverpool https://doi.org/10.1080/17445647.2022.2153091 2023-08-10T22:28:13Z We present the first extensive high-resolution glacial geomorphic map west of the Andean Cordillera in southernmost Chile (52.8–53.1°S, 73.0–73.9°W). The map extends over 1565 km2 and is based on high-resolution satellite images and aerial photographs. At selected locations, the remotely mapped geomorphology was corroborated by field observations. The study area is dominated by glacial erosional landforms (77%) over depositional landforms (23%), with published submarine depositional landforms having been included (e.g. moraines). Glacial drift, kettle kame topography and lateral and frontal moraines form the primary depositional landforms and sediment associations. Glacial cirques, wide U-shaped valleys, whalebacks, roches moutonnées and scoured bedrock characterize most of the mapped area. The spatial distribution of whalebacks and roches moutonnées in the study area indicates a lack of lithological control on their formation and a warm-based, dynamic ice velocity and thickness regime during Patagonian Ice Sheet cover and retreat during the last glacial cycle. Article in Journal/Newspaper Ice Sheet The University of Liverpool Repository Estrecho ENVELOPE(-60.783,-60.783,-62.467,-62.467) Magallanes ENVELOPE(-62.933,-62.933,-64.883,-64.883) Journal of Maps 19 1
institution Open Polar
collection The University of Liverpool Repository
op_collection_id ftunivliverpool
language English
description We present the first extensive high-resolution glacial geomorphic map west of the Andean Cordillera in southernmost Chile (52.8–53.1°S, 73.0–73.9°W). The map extends over 1565 km2 and is based on high-resolution satellite images and aerial photographs. At selected locations, the remotely mapped geomorphology was corroborated by field observations. The study area is dominated by glacial erosional landforms (77%) over depositional landforms (23%), with published submarine depositional landforms having been included (e.g. moraines). Glacial drift, kettle kame topography and lateral and frontal moraines form the primary depositional landforms and sediment associations. Glacial cirques, wide U-shaped valleys, whalebacks, roches moutonnées and scoured bedrock characterize most of the mapped area. The spatial distribution of whalebacks and roches moutonnées in the study area indicates a lack of lithological control on their formation and a warm-based, dynamic ice velocity and thickness regime during Patagonian Ice Sheet cover and retreat during the last glacial cycle.
format Article in Journal/Newspaper
author Smedley, Rachel
spellingShingle Smedley, Rachel
Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
author_facet Smedley, Rachel
author_sort Smedley, Rachel
title Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
title_short Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
title_full Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
title_fullStr Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
title_full_unstemmed Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W)
title_sort glacial geomorphology between the gran campo nevado and estrecho de magallanes, chile (52–53°s, 73°w)
publisher Taylor & Francis Group
publishDate 2023
url http://livrepository.liverpool.ac.uk/3170138/
https://doi.org/10.1080/17445647.2022.2153091
long_lat ENVELOPE(-60.783,-60.783,-62.467,-62.467)
ENVELOPE(-62.933,-62.933,-64.883,-64.883)
geographic Estrecho
Magallanes
geographic_facet Estrecho
Magallanes
genre Ice Sheet
genre_facet Ice Sheet
op_relation Smedley, Rachel orcid:0000-0001-7773-5193 (2023) Glacial geomorphology between the Gran Campo Nevado and Estrecho de Magallanes, Chile (52–53°S, 73°W). Journal of Maps, 19 (1). pp. 1-14.
op_doi https://doi.org/10.1080/17445647.2022.2153091
container_title Journal of Maps
container_volume 19
container_issue 1
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