Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough

The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analyses of sediment gravity cores from Store Koldewey Troug...

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Published in:The Cryosphere
Main Authors: Olsen, Ingrid Leirvik, Rydningen, Tom Arne, Forwick, Matthias, Laberg, Jan Sverre, Husum, Katrine
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-4475-2020
https://tc.copernicus.org/articles/14/4475/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:tc81774 2023-05-15T16:19:43+02:00 Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough Olsen, Ingrid Leirvik Rydningen, Tom Arne Forwick, Matthias Laberg, Jan Sverre Husum, Katrine 2020-12-04 application/pdf https://doi.org/10.5194/tc-14-4475-2020 https://tc.copernicus.org/articles/14/4475/2020/ eng eng doi:10.5194/tc-14-4475-2020 https://tc.copernicus.org/articles/14/4475/2020/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-14-4475-2020 2020-12-07T17:22:16Z The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analyses of sediment gravity cores from Store Koldewey Trough. Subglacial till fills the trough, with an overlying drape of maximum 2.5 m thick glacier-proximal and glacier-distal sediment. The presence of mega-scale glacial lineations and a grounding zone wedge in the outer part of the trough, comprising subglacial till, provides evidence of the expansion of fast-flowing, grounded ice, probably originating from the area presently covered with the Storstrømmen ice stream and thereby previously flowing across Store Koldewey Island and Germania Land. Grounding zone wedges and recessional moraines provide evidence that multiple halts and/or readvances interrupted the deglaciation. The formation of the grounding zone wedges is estimated to be at least 130 years, while distances between the recessional moraines indicate that the grounding line locally retreated between 80 and 400 m yr −1 during the deglaciation, assuming that the moraines formed annually. The complex geomorphology in Store Koldewey Trough is attributed to the trough shallowing and narrowing towards the coast. At a late stage of the deglaciation, the ice stream flowed around the topography on Store Koldewey Island and Germania Land, terminating the sediment input from this sector of the Greenland Ice Sheet to Store Koldewey Trough. Text Germania land glacier Greenland Ice Sheet Koldewey island Store koldewey Copernicus Publications: E-Journals Germania Land ENVELOPE(-20.042,-20.042,77.129,77.129) Greenland Store Koldewey ENVELOPE(-18.820,-18.820,76.364,76.364) The Cryosphere 14 12 4475 4494
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analyses of sediment gravity cores from Store Koldewey Trough. Subglacial till fills the trough, with an overlying drape of maximum 2.5 m thick glacier-proximal and glacier-distal sediment. The presence of mega-scale glacial lineations and a grounding zone wedge in the outer part of the trough, comprising subglacial till, provides evidence of the expansion of fast-flowing, grounded ice, probably originating from the area presently covered with the Storstrømmen ice stream and thereby previously flowing across Store Koldewey Island and Germania Land. Grounding zone wedges and recessional moraines provide evidence that multiple halts and/or readvances interrupted the deglaciation. The formation of the grounding zone wedges is estimated to be at least 130 years, while distances between the recessional moraines indicate that the grounding line locally retreated between 80 and 400 m yr −1 during the deglaciation, assuming that the moraines formed annually. The complex geomorphology in Store Koldewey Trough is attributed to the trough shallowing and narrowing towards the coast. At a late stage of the deglaciation, the ice stream flowed around the topography on Store Koldewey Island and Germania Land, terminating the sediment input from this sector of the Greenland Ice Sheet to Store Koldewey Trough.
format Text
author Olsen, Ingrid Leirvik
Rydningen, Tom Arne
Forwick, Matthias
Laberg, Jan Sverre
Husum, Katrine
spellingShingle Olsen, Ingrid Leirvik
Rydningen, Tom Arne
Forwick, Matthias
Laberg, Jan Sverre
Husum, Katrine
Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
author_facet Olsen, Ingrid Leirvik
Rydningen, Tom Arne
Forwick, Matthias
Laberg, Jan Sverre
Husum, Katrine
author_sort Olsen, Ingrid Leirvik
title Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
title_short Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
title_full Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
title_fullStr Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
title_full_unstemmed Last glacial ice sheet dynamics offshore NE Greenland – a case study from Store Koldewey Trough
title_sort last glacial ice sheet dynamics offshore ne greenland – a case study from store koldewey trough
publishDate 2020
url https://doi.org/10.5194/tc-14-4475-2020
https://tc.copernicus.org/articles/14/4475/2020/
long_lat ENVELOPE(-20.042,-20.042,77.129,77.129)
ENVELOPE(-18.820,-18.820,76.364,76.364)
geographic Germania Land
Greenland
Store Koldewey
geographic_facet Germania Land
Greenland
Store Koldewey
genre Germania land
glacier
Greenland
Ice Sheet
Koldewey island
Store koldewey
genre_facet Germania land
glacier
Greenland
Ice Sheet
Koldewey island
Store koldewey
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-14-4475-2020
https://tc.copernicus.org/articles/14/4475/2020/
op_doi https://doi.org/10.5194/tc-14-4475-2020
container_title The Cryosphere
container_volume 14
container_issue 12
container_start_page 4475
op_container_end_page 4494
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