Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm

Geologic and geomorphologic research in the Lisbet Valley (Lisbetdalen) and Kulmstranda proved a glaciation of the southern coast of Hornsund during the Würm (Vistulian) Glaciation. Maximum of this glaciation, expressed by an advance of glaciers in Hornsund, occurred about 45-40 000 years BP. An ear...

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Main Authors: Kłysz, Piotr, Lindner, Leszek
Format: Article in Journal/Newspaper
Language:English
Published: Faculty of Geology University of Warsaw 1981
Subjects:
Hornsund
Spitsbergen
Online Access:https://gq.pgi.gov.pl/agp/article/view/9435
id ftjgq:oai:geojournals.pgi.gov.pl:article/9435
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spelling ftjgq:oai:geojournals.pgi.gov.pl:article/9435 2024-09-15T18:10:56+00:00 Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm Kłysz, Piotr Lindner, Leszek 1981-06-30 application/pdf https://gq.pgi.gov.pl/agp/article/view/9435 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/9435/7983 https://gq.pgi.gov.pl/agp/article/view/9435 Acta Geologica Polonica; Vol. 31 No. 1-2 (1981); 139-150 Acta Geologica Polonica; Tom 31 Nr 1-2 (1981); 139-150 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1981 ftjgq 2024-07-30T03:29:09Z Geologic and geomorphologic research in the Lisbet Valley (Lisbetdalen) and Kulmstranda proved a glaciation of the southern coast of Hornsund during the Würm (Vistulian) Glaciation. Maximum of this glaciation, expressed by an advance of glaciers in Hornsund, occurred about 45-40 000 years BP. An early retreat stage of the ·glaciers, marked among others by the highest marine terrace (80-100 m a.s.l.) took place about 25-20 000 years BP. Article in Journal/Newspaper Hornsund Spitsbergen Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
description Geologic and geomorphologic research in the Lisbet Valley (Lisbetdalen) and Kulmstranda proved a glaciation of the southern coast of Hornsund during the Würm (Vistulian) Glaciation. Maximum of this glaciation, expressed by an advance of glaciers in Hornsund, occurred about 45-40 000 years BP. An early retreat stage of the ·glaciers, marked among others by the highest marine terrace (80-100 m a.s.l.) took place about 25-20 000 years BP.
format Article in Journal/Newspaper
author Kłysz, Piotr
Lindner, Leszek
spellingShingle Kłysz, Piotr
Lindner, Leszek
Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
author_facet Kłysz, Piotr
Lindner, Leszek
author_sort Kłysz, Piotr
title Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
title_short Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
title_full Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
title_fullStr Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
title_full_unstemmed Development of glaciers on the southern coast of Hornsund in Spitsbergen during the Würm
title_sort development of glaciers on the southern coast of hornsund in spitsbergen during the würm
publisher Faculty of Geology University of Warsaw
publishDate 1981
url https://gq.pgi.gov.pl/agp/article/view/9435
genre Hornsund
Spitsbergen
genre_facet Hornsund
Spitsbergen
op_source Acta Geologica Polonica; Vol. 31 No. 1-2 (1981); 139-150
Acta Geologica Polonica; Tom 31 Nr 1-2 (1981); 139-150
op_relation https://gq.pgi.gov.pl/agp/article/view/9435/7983
https://gq.pgi.gov.pl/agp/article/view/9435
_version_ 1810448519104823296

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