Neoglacial glacier changes around Storstrommen, North-East Greenland
Early Holocene recession of the ice cover over Germania Land in North-East Greenland 7.5 ka B.P. brought the Inland Ice margin back to a position close to the present. Continued recessions after that time lead to the formation of a "Storstrømmen Sound" which separated Germania Land from ma...
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ftawi:oai:epic.awi.de:3306 2024-09-15T18:04:15+00:00 Neoglacial glacier changes around Storstrommen, North-East Greenland Weidick, A. Andreasen, C. Oerter, Hans Reeh, N. 1996 https://epic.awi.de/id/eprint/3306/ https://hdl.handle.net/10013/epic.13889 unknown Weidick, A. , Andreasen, C. , Oerter, H. and Reeh, N. (1996) Neoglacial glacier changes around Storstrommen, North-East Greenland , Polarforschung, 64 (3), pp. 95-108 . hdl:10013/epic.13889 EPIC3Polarforschung, 64(3), pp. 95-108, ISSN: 0032-249 Article peerRev 1996 ftawi 2024-06-24T03:54:11Z Early Holocene recession of the ice cover over Germania Land in North-East Greenland 7.5 ka B.P. brought the Inland Ice margin back to a position close to the present. Continued recessions after that time lead to the formation of a "Storstrømmen Sound" which separated Germania Land from mainland Greenland in the period from about 6 to 1 ka B.P. The present filling of the approximately 100 km long sound by the glaciers of Storstrømmen and Kofoed-Hansen Brae must therefore have taken place during the Little Ice Age. In an archaeological sense this implies deterioration of the living conditions of Neo-Eskimos compared to those of Palaeo-Eskimos.The neoglacial re-formation and present existence of the glaciers as a Little Ice Age relict may imply a present-day instability in their dynamics, as demonstrated by the pulsations (surge-like behaviour) in the last part of the 20th century. An earlier Little Ice Age advance might possibly have had the same amplitude as that documented from the 20th century but its exact age and character is not known.The glacio-isostatic response of the earth's crust to the variations in the Holocene glacier load implies a relatively slow and slight emergence and subsequent submergence. The shift from emergence to submergence must have taken place between about 2 and 1 ka B.P. Article in Journal/Newspaper East Greenland eskimo* Germania land glacier Greenland Polarforschung Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
Early Holocene recession of the ice cover over Germania Land in North-East Greenland 7.5 ka B.P. brought the Inland Ice margin back to a position close to the present. Continued recessions after that time lead to the formation of a "Storstrømmen Sound" which separated Germania Land from mainland Greenland in the period from about 6 to 1 ka B.P. The present filling of the approximately 100 km long sound by the glaciers of Storstrømmen and Kofoed-Hansen Brae must therefore have taken place during the Little Ice Age. In an archaeological sense this implies deterioration of the living conditions of Neo-Eskimos compared to those of Palaeo-Eskimos.The neoglacial re-formation and present existence of the glaciers as a Little Ice Age relict may imply a present-day instability in their dynamics, as demonstrated by the pulsations (surge-like behaviour) in the last part of the 20th century. An earlier Little Ice Age advance might possibly have had the same amplitude as that documented from the 20th century but its exact age and character is not known.The glacio-isostatic response of the earth's crust to the variations in the Holocene glacier load implies a relatively slow and slight emergence and subsequent submergence. The shift from emergence to submergence must have taken place between about 2 and 1 ka B.P. |
format |
Article in Journal/Newspaper |
author |
Weidick, A. Andreasen, C. Oerter, Hans Reeh, N. |
spellingShingle |
Weidick, A. Andreasen, C. Oerter, Hans Reeh, N. Neoglacial glacier changes around Storstrommen, North-East Greenland |
author_facet |
Weidick, A. Andreasen, C. Oerter, Hans Reeh, N. |
author_sort |
Weidick, A. |
title |
Neoglacial glacier changes around Storstrommen, North-East Greenland |
title_short |
Neoglacial glacier changes around Storstrommen, North-East Greenland |
title_full |
Neoglacial glacier changes around Storstrommen, North-East Greenland |
title_fullStr |
Neoglacial glacier changes around Storstrommen, North-East Greenland |
title_full_unstemmed |
Neoglacial glacier changes around Storstrommen, North-East Greenland |
title_sort |
neoglacial glacier changes around storstrommen, north-east greenland |
publishDate |
1996 |
url |
https://epic.awi.de/id/eprint/3306/ https://hdl.handle.net/10013/epic.13889 |
genre |
East Greenland eskimo* Germania land glacier Greenland Polarforschung |
genre_facet |
East Greenland eskimo* Germania land glacier Greenland Polarforschung |
op_source |
EPIC3Polarforschung, 64(3), pp. 95-108, ISSN: 0032-249 |
op_relation |
Weidick, A. , Andreasen, C. , Oerter, H. and Reeh, N. (1996) Neoglacial glacier changes around Storstrommen, North-East Greenland , Polarforschung, 64 (3), pp. 95-108 . hdl:10013/epic.13889 |
_version_ |
1810441755148943360 |