An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard
A 20 m thick shallow marine sequence, capped by a Late Weichselian lodgement till, is exposed for 200111 along the river in Linnedalen on the west coast of Svalbard. Five formations are recognized: Formation A, the oldest, consists of a shallow marine, proglacial fan, of channelized sandy turbidites...
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crwiley:10.1111/j.1502-3885.1991.tb00298.x 2024-09-15T18:07:55+00:00 An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard LONNE, IDA MANGERUD, JAN 1991 http://dx.doi.org/10.1111/j.1502-3885.1991.tb00298.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1991.tb00298.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1991.tb00298.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 20, issue 2, page 85-104 ISSN 0300-9483 1502-3885 journal-article 1991 crwiley https://doi.org/10.1111/j.1502-3885.1991.tb00298.x 2024-07-25T04:21:03Z A 20 m thick shallow marine sequence, capped by a Late Weichselian lodgement till, is exposed for 200111 along the river in Linnedalen on the west coast of Svalbard. Five formations are recognized: Formation A, the oldest, consists of a shallow marine, proglacial fan, of channelized sandy turbidites, possibly fed from an ice‐contact deposit. Formation B, a sequence of proglacial channels and ice‐rafted debris, was formed during a small oscillation of the glacier. Formation C, a prograding, storm‐dominated shoreline sequence, was formed during a sea level fall, assumed to be a result of glacio‐isostatic uplift. Formation D, a lodgement till formed during the last glacier advance in Linnedalen and formation E, a coarsening upwards sequence, were formed during the post‐glacial sea level fall. The subtill sequence (fm. A, B and C) is dated to between 40,000BP (radiocarbon dates) and 120,000BP (thermoluminescence and amino acid D/L ratios). The glacier front was 10 km downvalley during deposition of formations A and B, relative to the present glacier terminus, and more than 12km during the late Weichselian maximum. Article in Journal/Newspaper glacier Svalbard Wiley Online Library Boreas 20 2 85 104 |
institution |
Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
A 20 m thick shallow marine sequence, capped by a Late Weichselian lodgement till, is exposed for 200111 along the river in Linnedalen on the west coast of Svalbard. Five formations are recognized: Formation A, the oldest, consists of a shallow marine, proglacial fan, of channelized sandy turbidites, possibly fed from an ice‐contact deposit. Formation B, a sequence of proglacial channels and ice‐rafted debris, was formed during a small oscillation of the glacier. Formation C, a prograding, storm‐dominated shoreline sequence, was formed during a sea level fall, assumed to be a result of glacio‐isostatic uplift. Formation D, a lodgement till formed during the last glacier advance in Linnedalen and formation E, a coarsening upwards sequence, were formed during the post‐glacial sea level fall. The subtill sequence (fm. A, B and C) is dated to between 40,000BP (radiocarbon dates) and 120,000BP (thermoluminescence and amino acid D/L ratios). The glacier front was 10 km downvalley during deposition of formations A and B, relative to the present glacier terminus, and more than 12km during the late Weichselian maximum. |
format |
Article in Journal/Newspaper |
author |
LONNE, IDA MANGERUD, JAN |
spellingShingle |
LONNE, IDA MANGERUD, JAN An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
author_facet |
LONNE, IDA MANGERUD, JAN |
author_sort |
LONNE, IDA |
title |
An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
title_short |
An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
title_full |
An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
title_fullStr |
An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
title_full_unstemmed |
An Early or Middle Weichselian sequence of proglacial, shallow marine sediments on western Svalbard |
title_sort |
early or middle weichselian sequence of proglacial, shallow marine sediments on western svalbard |
publisher |
Wiley |
publishDate |
1991 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1991.tb00298.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1991.tb00298.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1991.tb00298.x |
genre |
glacier Svalbard |
genre_facet |
glacier Svalbard |
op_source |
Boreas volume 20, issue 2, page 85-104 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1991.tb00298.x |
container_title |
Boreas |
container_volume |
20 |
container_issue |
2 |
container_start_page |
85 |
op_container_end_page |
104 |
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1810445284802560000 |