Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation

The Greenland ice sheet (GrIS) covers a complex network of canyons thought to be preglacial and fluvial in origin, implying that these features have influenced the ice sheet since its inception. The largest of these canyons terminates in northwest Greenland at the outlet of the Petermann Glacier. Ye...

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Published in:Geology
Main Authors: Keisling, B.A., Nielsen, Lisbeth Tangaa, Hvidberg, Christine Schøtt, Nuterman, Roman, DeConto, Robert M.
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://curis.ku.dk/portal/da/publications/pliocenepleistocene-megafloods-as-a-mechanism-for-greenlandic-megacanyon-formation(c33be04e-f304-4c9e-a0ac-db8847dab834).html
https://doi.org/10.1130/G47253.1
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spelling ftcopenhagenunip:oai:pure.atira.dk:publications/c33be04e-f304-4c9e-a0ac-db8847dab834 2024-04-28T08:19:52+00:00 Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation Keisling, B.A. Nielsen, Lisbeth Tangaa Hvidberg, Christine Schøtt Nuterman, Roman DeConto, Robert M. 2020-04-29 https://curis.ku.dk/portal/da/publications/pliocenepleistocene-megafloods-as-a-mechanism-for-greenlandic-megacanyon-formation(c33be04e-f304-4c9e-a0ac-db8847dab834).html https://doi.org/10.1130/G47253.1 eng eng info:eu-repo/semantics/closedAccess Keisling , B A , Nielsen , L T , Hvidberg , C S , Nuterman , R & DeConto , R M 2020 , ' Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation ' , Geology , vol. 48 , no. 7 , pp. 737-741 . https://doi.org/10.1130/G47253.1 article 2020 ftcopenhagenunip https://doi.org/10.1130/G47253.1 2024-04-11T00:22:40Z The Greenland ice sheet (GrIS) covers a complex network of canyons thought to be preglacial and fluvial in origin, implying that these features have influenced the ice sheet since its inception. The largest of these canyons terminates in northwest Greenland at the outlet of the Petermann Glacier. Yet, the genesis of this canyon, and similar features in northern Greenland, remains unknown. Here, we present numerical model simulations of early GrIS history and show that interactions among climate, the growing ice sheet, and preexisting topography may have contributed to the excavation of the canyon via repeated catastrophic outburst floods. Our results have implications for interpreting sedimentary and geomorphic features beneath the GrIS and around its marine margins, and they document a novel mechanism for landscape erosion in Greenland. Article in Journal/Newspaper glacier Greenland greenlandic Ice Sheet Petermann glacier University of Copenhagen: Research Geology 48 7 737 741
institution Open Polar
collection University of Copenhagen: Research
op_collection_id ftcopenhagenunip
language English
description The Greenland ice sheet (GrIS) covers a complex network of canyons thought to be preglacial and fluvial in origin, implying that these features have influenced the ice sheet since its inception. The largest of these canyons terminates in northwest Greenland at the outlet of the Petermann Glacier. Yet, the genesis of this canyon, and similar features in northern Greenland, remains unknown. Here, we present numerical model simulations of early GrIS history and show that interactions among climate, the growing ice sheet, and preexisting topography may have contributed to the excavation of the canyon via repeated catastrophic outburst floods. Our results have implications for interpreting sedimentary and geomorphic features beneath the GrIS and around its marine margins, and they document a novel mechanism for landscape erosion in Greenland.
format Article in Journal/Newspaper
author Keisling, B.A.
Nielsen, Lisbeth Tangaa
Hvidberg, Christine Schøtt
Nuterman, Roman
DeConto, Robert M.
spellingShingle Keisling, B.A.
Nielsen, Lisbeth Tangaa
Hvidberg, Christine Schøtt
Nuterman, Roman
DeConto, Robert M.
Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
author_facet Keisling, B.A.
Nielsen, Lisbeth Tangaa
Hvidberg, Christine Schøtt
Nuterman, Roman
DeConto, Robert M.
author_sort Keisling, B.A.
title Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
title_short Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
title_full Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
title_fullStr Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
title_full_unstemmed Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation
title_sort pliocene–pleistocene megafloods as a mechanism for greenlandic megacanyon formation
publishDate 2020
url https://curis.ku.dk/portal/da/publications/pliocenepleistocene-megafloods-as-a-mechanism-for-greenlandic-megacanyon-formation(c33be04e-f304-4c9e-a0ac-db8847dab834).html
https://doi.org/10.1130/G47253.1
genre glacier
Greenland
greenlandic
Ice Sheet
Petermann glacier
genre_facet glacier
Greenland
greenlandic
Ice Sheet
Petermann glacier
op_source Keisling , B A , Nielsen , L T , Hvidberg , C S , Nuterman , R & DeConto , R M 2020 , ' Pliocene–Pleistocene megafloods as a mechanism for Greenlandic megacanyon formation ' , Geology , vol. 48 , no. 7 , pp. 737-741 . https://doi.org/10.1130/G47253.1
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1130/G47253.1
container_title Geology
container_volume 48
container_issue 7
container_start_page 737
op_container_end_page 741
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