The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age
We present glacial geologic and chronologic data concerning the Holocene ice extent in the Stauning Alper of East Greenland. The retreat of ice from the late-glacial position back into the mountains was accomplished by at least 11 000 cal years B.P. The only recorded advance after this time occurred...
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Norwegian Polar Institute
2008
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ftjpolarres:oai:journals.openacademia.net:article/2878 2023-05-15T14:24:18+02:00 The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age Hall, Brenda L. Baroni, Carlo Denton, George H. 2008-08-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2878 https://doi.org/10.3402/polar.v27i2.6171 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2878/6505 https://polarresearch.net/index.php/polar/article/view/2878 doi:10.3402/polar.v27i2.6171 Copyright (c) 2018 Polar Research Polar Research; Vol. 27 No. 2 (2008): Special issue: Arctic Palaeoclimate and its Extremes (APEX); 128-134 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2008 ftjpolarres https://doi.org/10.3402/polar.v27i2.6171 2021-11-11T19:13:21Z We present glacial geologic and chronologic data concerning the Holocene ice extent in the Stauning Alper of East Greenland. The retreat of ice from the late-glacial position back into the mountains was accomplished by at least 11 000 cal years B.P. The only recorded advance after this time occurred during the past few centuries (the Little Ice Age). Therefore, we postulate that the Little Ice Age event represents the maximum Holocene ice extent in this part of East Greenland. Article in Journal/Newspaper Arctic East Greenland Greenland Polar Research Polar Research (E-Journal) Greenland Stauning Alper ENVELOPE(-25.167,-25.167,72.000,72.000) Polar Research 27 2 |
institution |
Open Polar |
collection |
Polar Research (E-Journal) |
op_collection_id |
ftjpolarres |
language |
English |
description |
We present glacial geologic and chronologic data concerning the Holocene ice extent in the Stauning Alper of East Greenland. The retreat of ice from the late-glacial position back into the mountains was accomplished by at least 11 000 cal years B.P. The only recorded advance after this time occurred during the past few centuries (the Little Ice Age). Therefore, we postulate that the Little Ice Age event represents the maximum Holocene ice extent in this part of East Greenland. |
format |
Article in Journal/Newspaper |
author |
Hall, Brenda L. Baroni, Carlo Denton, George H. |
spellingShingle |
Hall, Brenda L. Baroni, Carlo Denton, George H. The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
author_facet |
Hall, Brenda L. Baroni, Carlo Denton, George H. |
author_sort |
Hall, Brenda L. |
title |
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
title_short |
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
title_full |
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
title_fullStr |
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
title_full_unstemmed |
The most extensive Holocene advance in the Stauning Alper, East Greenland, occurred in the Little Ice Age |
title_sort |
most extensive holocene advance in the stauning alper, east greenland, occurred in the little ice age |
publisher |
Norwegian Polar Institute |
publishDate |
2008 |
url |
https://polarresearch.net/index.php/polar/article/view/2878 https://doi.org/10.3402/polar.v27i2.6171 |
long_lat |
ENVELOPE(-25.167,-25.167,72.000,72.000) |
geographic |
Greenland Stauning Alper |
geographic_facet |
Greenland Stauning Alper |
genre |
Arctic East Greenland Greenland Polar Research |
genre_facet |
Arctic East Greenland Greenland Polar Research |
op_source |
Polar Research; Vol. 27 No. 2 (2008): Special issue: Arctic Palaeoclimate and its Extremes (APEX); 128-134 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2878/6505 https://polarresearch.net/index.php/polar/article/view/2878 doi:10.3402/polar.v27i2.6171 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v27i2.6171 |
container_title |
Polar Research |
container_volume |
27 |
container_issue |
2 |
_version_ |
1766296731097497600 |