Late Quaternary glaciation in the south‐western Barents Sea

Moraine ridges have been morphologically and seismically identified in the south‐western Barents Sea. Some of these ridges were deposited in front of ice lobes from the northern part of the Fennoscandian Ice Sheet, others in front of glaciers located on the southern Barents Sea shelf. The moraine ri...

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Published in:Boreas
Main Authors: VORREN, TORE O., KRISTOFFERSEN, YNGVE
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1986
Subjects:
Barents Sea
Fennoscandian
Ice Sheet
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1986.tb00742.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1986.tb00742.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1986.tb00742.x
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spelling crwiley:10.1111/j.1502-3885.1986.tb00742.x 2024-06-02T08:04:05+00:00 Late Quaternary glaciation in the south‐western Barents Sea VORREN, TORE O. KRISTOFFERSEN, YNGVE 1986 http://dx.doi.org/10.1111/j.1502-3885.1986.tb00742.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1986.tb00742.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1986.tb00742.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 15, issue 1, page 51-59 ISSN 0300-9483 1502-3885 journal-article 1986 crwiley https://doi.org/10.1111/j.1502-3885.1986.tb00742.x 2024-05-03T10:38:53Z Moraine ridges have been morphologically and seismically identified in the south‐western Barents Sea. Some of these ridges were deposited in front of ice lobes from the northern part of the Fennoscandian Ice Sheet, others in front of glaciers located on the southern Barents Sea shelf. The moraine ridges were probably deposited during the Weichselian, possibly the Late Weichselian. Article in Journal/Newspaper Barents Sea Fennoscandian Ice Sheet Wiley Online Library Barents Sea Boreas 15 1 51 59
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Moraine ridges have been morphologically and seismically identified in the south‐western Barents Sea. Some of these ridges were deposited in front of ice lobes from the northern part of the Fennoscandian Ice Sheet, others in front of glaciers located on the southern Barents Sea shelf. The moraine ridges were probably deposited during the Weichselian, possibly the Late Weichselian.
format Article in Journal/Newspaper
author VORREN, TORE O.
KRISTOFFERSEN, YNGVE
spellingShingle VORREN, TORE O.
KRISTOFFERSEN, YNGVE
Late Quaternary glaciation in the south‐western Barents Sea
author_facet VORREN, TORE O.
KRISTOFFERSEN, YNGVE
author_sort VORREN, TORE O.
title Late Quaternary glaciation in the south‐western Barents Sea
title_short Late Quaternary glaciation in the south‐western Barents Sea
title_full Late Quaternary glaciation in the south‐western Barents Sea
title_fullStr Late Quaternary glaciation in the south‐western Barents Sea
title_full_unstemmed Late Quaternary glaciation in the south‐western Barents Sea
title_sort late quaternary glaciation in the south‐western barents sea
publisher Wiley
publishDate 1986
url http://dx.doi.org/10.1111/j.1502-3885.1986.tb00742.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1986.tb00742.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1986.tb00742.x
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
Fennoscandian
Ice Sheet
genre_facet Barents Sea
Fennoscandian
Ice Sheet
op_source Boreas
volume 15, issue 1, page 51-59
ISSN 0300-9483 1502-3885
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1502-3885.1986.tb00742.x
container_title Boreas
container_volume 15
container_issue 1
container_start_page 51
op_container_end_page 59
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