Offshore sedimentation in the Hyttevika Bay, South Spitsbergen

In the intertidal and offshore zones of the Hyttevika Bay (South Spitsbergen) two phases of deposition are recognizable. During the first one, the accumulation results from melting of sea ice blocks and a calf ice whereas during the second phase the successive generations of beach ridges and beach s...

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Main Authors: Giżejewski, Jerzy, Roszczynko, Waldemar
Format: Article in Journal/Newspaper
Language:English
Published: Faculty of Geology University of Warsaw 1982
Subjects:
Sea ice
Spitsbergen
Online Access:https://gq.pgi.gov.pl/agp/article/view/9530
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spelling ftjgq:oai:geojournals.pgi.gov.pl:article/9530 2024-09-15T18:35:15+00:00 Offshore sedimentation in the Hyttevika Bay, South Spitsbergen Giżejewski, Jerzy Roszczynko, Waldemar 1982-12-29 application/pdf https://gq.pgi.gov.pl/agp/article/view/9530 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/9530/8078 https://gq.pgi.gov.pl/agp/article/view/9530 Acta Geologica Polonica; Vol. 32 No. 3-4 (1982); 279-288 Acta Geologica Polonica; Tom 32 Nr 3-4 (1982); 279-288 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1982 ftjgq 2024-07-30T03:29:09Z In the intertidal and offshore zones of the Hyttevika Bay (South Spitsbergen) two phases of deposition are recognizable. During the first one, the accumulation results from melting of sea ice blocks and a calf ice whereas during the second phase the successive generations of beach ridges and beach sediments are formed in a shallow offshore zone. These phases are noted in raised marine terraces as a bipartity of their sediments. Basing on that, an evolution model of the sediments of raised marine terraces and discussion on their age are presented. Article in Journal/Newspaper Sea ice Spitsbergen Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
description In the intertidal and offshore zones of the Hyttevika Bay (South Spitsbergen) two phases of deposition are recognizable. During the first one, the accumulation results from melting of sea ice blocks and a calf ice whereas during the second phase the successive generations of beach ridges and beach sediments are formed in a shallow offshore zone. These phases are noted in raised marine terraces as a bipartity of their sediments. Basing on that, an evolution model of the sediments of raised marine terraces and discussion on their age are presented.
format Article in Journal/Newspaper
author Giżejewski, Jerzy
Roszczynko, Waldemar
spellingShingle Giżejewski, Jerzy
Roszczynko, Waldemar
Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
author_facet Giżejewski, Jerzy
Roszczynko, Waldemar
author_sort Giżejewski, Jerzy
title Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
title_short Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
title_full Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
title_fullStr Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
title_full_unstemmed Offshore sedimentation in the Hyttevika Bay, South Spitsbergen
title_sort offshore sedimentation in the hyttevika bay, south spitsbergen
publisher Faculty of Geology University of Warsaw
publishDate 1982
url https://gq.pgi.gov.pl/agp/article/view/9530
genre Sea ice
Spitsbergen
genre_facet Sea ice
Spitsbergen
op_source Acta Geologica Polonica; Vol. 32 No. 3-4 (1982); 279-288
Acta Geologica Polonica; Tom 32 Nr 3-4 (1982); 279-288
op_relation https://gq.pgi.gov.pl/agp/article/view/9530/8078
https://gq.pgi.gov.pl/agp/article/view/9530
_version_ 1810478285697581056

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