Late‐glacial marine erosion in Scotland
A pronouaced raised reck platform and cliff that occur on part of the west coast of Scotland ale generally considered to have been formed before the last glaciation. It is argued in this paper that they were formed in late‐glacial times, mainly during the Loch Lomond (Upper Dryas) Readvance. The fea...
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Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1974.tb00826.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1974.tb00826.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1974.tb00826.x |
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crwiley:10.1111/j.1502-3885.1974.tb00826.x 2024-09-15T18:25:49+00:00 Late‐glacial marine erosion in Scotland SISSONS, J. BRIAN 1974 http://dx.doi.org/10.1111/j.1502-3885.1974.tb00826.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1974.tb00826.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1974.tb00826.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 3, issue 2, page 41-48 ISSN 0300-9483 1502-3885 journal-article 1974 crwiley https://doi.org/10.1111/j.1502-3885.1974.tb00826.x 2024-07-25T04:21:58Z A pronouaced raised reck platform and cliff that occur on part of the west coast of Scotland ale generally considered to have been formed before the last glaciation. It is argued in this paper that they were formed in late‐glacial times, mainly during the Loch Lomond (Upper Dryas) Readvance. The features arc correlated with an extensive buried and/or submerged marine erosion feature in South‐East Scotland. It is also suggested that the Scottish features correlate with the ‘Main line’ (P 12 shoreline) of northern Norway. Article in Journal/Newspaper Northern Norway Wiley Online Library Boreas 3 2 41 48 |
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crwiley |
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English |
description |
A pronouaced raised reck platform and cliff that occur on part of the west coast of Scotland ale generally considered to have been formed before the last glaciation. It is argued in this paper that they were formed in late‐glacial times, mainly during the Loch Lomond (Upper Dryas) Readvance. The features arc correlated with an extensive buried and/or submerged marine erosion feature in South‐East Scotland. It is also suggested that the Scottish features correlate with the ‘Main line’ (P 12 shoreline) of northern Norway. |
format |
Article in Journal/Newspaper |
author |
SISSONS, J. BRIAN |
spellingShingle |
SISSONS, J. BRIAN Late‐glacial marine erosion in Scotland |
author_facet |
SISSONS, J. BRIAN |
author_sort |
SISSONS, J. BRIAN |
title |
Late‐glacial marine erosion in Scotland |
title_short |
Late‐glacial marine erosion in Scotland |
title_full |
Late‐glacial marine erosion in Scotland |
title_fullStr |
Late‐glacial marine erosion in Scotland |
title_full_unstemmed |
Late‐glacial marine erosion in Scotland |
title_sort |
late‐glacial marine erosion in scotland |
publisher |
Wiley |
publishDate |
1974 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1974.tb00826.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1974.tb00826.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1974.tb00826.x |
genre |
Northern Norway |
genre_facet |
Northern Norway |
op_source |
Boreas volume 3, issue 2, page 41-48 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1974.tb00826.x |
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Boreas |
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3 |
container_issue |
2 |
container_start_page |
41 |
op_container_end_page |
48 |
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1810466281555492864 |