Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland

Earlier work in northeast Greenland has suggested a limited advance of the Greenland Ice Sheet during the Last Glacial Maximum (LGM). However, this concept has recently been challenged by marine geological studies, indicating grounded ice on the continental shelf at this time. New Be-10-ages from th...

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Published in:Geografiska Annaler: Series A, Physical Geography
Main Authors: Håkansson, Lena, Graf, A., Strasky, S., Ivy-Ochs, S., Kubik, P. W., Hjort, C., Schluchter, C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2007
Subjects:
Online Access:https://lup.lub.lu.se/record/1416790
https://doi.org/10.1111/j.1468-0459.2007.00318.x
id ftulundlup:oai:lup.lub.lu.se:0c698101-ff00-4db0-bdd1-189e94be125f
record_format openpolar
spelling ftulundlup:oai:lup.lub.lu.se:0c698101-ff00-4db0-bdd1-189e94be125f 2023-05-15T15:03:09+02:00 Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland Håkansson, Lena Graf, A. Strasky, S. Ivy-Ochs, S. Kubik, P. W. Hjort, C. Schluchter, C. 2007 https://lup.lub.lu.se/record/1416790 https://doi.org/10.1111/j.1468-0459.2007.00318.x eng eng Wiley-Blackwell https://lup.lub.lu.se/record/1416790 http://dx.doi.org/10.1111/j.1468-0459.2007.00318.x wos:000248959100004 scopus:34547885786 Geografiska Annaler. Series A. Physical Geography; 89A(3), pp 195-202 (2007) ISSN: 0435-3676 Geology NORTHERN EAST GREENLAND SOUTHERN ICE-SHEET greenland SCOTLAND MOUNTAINS EROSION LANDSCAPE EXPOSURE AGES LAST GLACIAL MAXIMUM ARCTIC CANADA NORWAY cosmogenic exposure dating blockfields contributiontojournal/article info:eu-repo/semantics/article text 2007 ftulundlup https://doi.org/10.1111/j.1468-0459.2007.00318.x 2023-02-01T23:28:42Z Earlier work in northeast Greenland has suggested a limited advance of the Greenland Ice Sheet during the Last Glacial Maximum (LGM). However, this concept has recently been challenged by marine geological studies, indicating grounded ice on the continental shelf at this time. New Be-10-ages from the Store Koldewey island, northeast Greenland, suggest that unscoured mountain plateaus at the outer coast were covered at least partly by cold-based ice during the LGM. It is, however, still inconclusive whether this ice was dynamically connected to the Greenland Ice Sheet or not. Regardless of the LGM ice sheet extent, the Be-10 results from Store Koldewey add to a growing body of evidence suggesting considerable antiquity of crystalline unscoured terrain near present and Pleistocene ice sheet margins. Article in Journal/Newspaper Arctic East Greenland Greenland Ice Sheet Koldewey island Store koldewey Lund University Publications (LUP) Arctic Canada Greenland Norway Store Koldewey ENVELOPE(-18.820,-18.820,76.364,76.364) Geografiska Annaler: Series A, Physical Geography 89 3 195 202
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Geology
NORTHERN EAST GREENLAND
SOUTHERN
ICE-SHEET
greenland
SCOTLAND
MOUNTAINS
EROSION
LANDSCAPE
EXPOSURE AGES
LAST GLACIAL MAXIMUM
ARCTIC CANADA
NORWAY
cosmogenic exposure dating
blockfields
spellingShingle Geology
NORTHERN EAST GREENLAND
SOUTHERN
ICE-SHEET
greenland
SCOTLAND
MOUNTAINS
EROSION
LANDSCAPE
EXPOSURE AGES
LAST GLACIAL MAXIMUM
ARCTIC CANADA
NORWAY
cosmogenic exposure dating
blockfields
Håkansson, Lena
Graf, A.
Strasky, S.
Ivy-Ochs, S.
Kubik, P. W.
Hjort, C.
Schluchter, C.
Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
topic_facet Geology
NORTHERN EAST GREENLAND
SOUTHERN
ICE-SHEET
greenland
SCOTLAND
MOUNTAINS
EROSION
LANDSCAPE
EXPOSURE AGES
LAST GLACIAL MAXIMUM
ARCTIC CANADA
NORWAY
cosmogenic exposure dating
blockfields
description Earlier work in northeast Greenland has suggested a limited advance of the Greenland Ice Sheet during the Last Glacial Maximum (LGM). However, this concept has recently been challenged by marine geological studies, indicating grounded ice on the continental shelf at this time. New Be-10-ages from the Store Koldewey island, northeast Greenland, suggest that unscoured mountain plateaus at the outer coast were covered at least partly by cold-based ice during the LGM. It is, however, still inconclusive whether this ice was dynamically connected to the Greenland Ice Sheet or not. Regardless of the LGM ice sheet extent, the Be-10 results from Store Koldewey add to a growing body of evidence suggesting considerable antiquity of crystalline unscoured terrain near present and Pleistocene ice sheet margins.
format Article in Journal/Newspaper
author Håkansson, Lena
Graf, A.
Strasky, S.
Ivy-Ochs, S.
Kubik, P. W.
Hjort, C.
Schluchter, C.
author_facet Håkansson, Lena
Graf, A.
Strasky, S.
Ivy-Ochs, S.
Kubik, P. W.
Hjort, C.
Schluchter, C.
author_sort Håkansson, Lena
title Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
title_short Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
title_full Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
title_fullStr Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
title_full_unstemmed Cosmogenic Be-10-ages from the Store Koldewey island, NE Greenland
title_sort cosmogenic be-10-ages from the store koldewey island, ne greenland
publisher Wiley-Blackwell
publishDate 2007
url https://lup.lub.lu.se/record/1416790
https://doi.org/10.1111/j.1468-0459.2007.00318.x
long_lat ENVELOPE(-18.820,-18.820,76.364,76.364)
geographic Arctic
Canada
Greenland
Norway
Store Koldewey
geographic_facet Arctic
Canada
Greenland
Norway
Store Koldewey
genre Arctic
East Greenland
Greenland
Ice Sheet
Koldewey island
Store koldewey
genre_facet Arctic
East Greenland
Greenland
Ice Sheet
Koldewey island
Store koldewey
op_source Geografiska Annaler. Series A. Physical Geography; 89A(3), pp 195-202 (2007)
ISSN: 0435-3676
op_relation https://lup.lub.lu.se/record/1416790
http://dx.doi.org/10.1111/j.1468-0459.2007.00318.x
wos:000248959100004
scopus:34547885786
op_doi https://doi.org/10.1111/j.1468-0459.2007.00318.x
container_title Geografiska Annaler: Series A, Physical Geography
container_volume 89
container_issue 3
container_start_page 195
op_container_end_page 202
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