Weichselian Convolution Phenomena and processes in fine sediments.
In three excavations in the southern Netherlands and northern Belgium, the Weichselian convolutions in fine sand, silt and clay deposits were investigated, and an attempt was made towards a semi‐quantitative approach to some sediment parameters. This, together with a detailed field survey, enabled i...
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crwiley:10.1111/j.1502-3885.1982.tb00539.x 2024-09-15T18:29:43+00:00 Weichselian Convolution Phenomena and processes in fine sediments. VANDENBERGHE, JEF BROEK, PETER VAN DEN 1982 http://dx.doi.org/10.1111/j.1502-3885.1982.tb00539.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1982.tb00539.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1982.tb00539.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 11, issue 4, page 299-315 ISSN 0300-9483 1502-3885 journal-article 1982 crwiley https://doi.org/10.1111/j.1502-3885.1982.tb00539.x 2024-07-25T04:21:52Z In three excavations in the southern Netherlands and northern Belgium, the Weichselian convolutions in fine sand, silt and clay deposits were investigated, and an attempt was made towards a semi‐quantitative approach to some sediment parameters. This, together with a detailed field survey, enabled interpretation of the deformations as forms of periglacial loadcasting. They originated from the time of permafrost degradation when large quantites of water were available. The amplitude of the involutions can be related to the depth of the permafrost table at that time. During the weichselian, two periods occurred in which this involution process could have been active Article in Journal/Newspaper permafrost Wiley Online Library Boreas 11 4 299 315 |
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Open Polar |
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Wiley Online Library |
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English |
description |
In three excavations in the southern Netherlands and northern Belgium, the Weichselian convolutions in fine sand, silt and clay deposits were investigated, and an attempt was made towards a semi‐quantitative approach to some sediment parameters. This, together with a detailed field survey, enabled interpretation of the deformations as forms of periglacial loadcasting. They originated from the time of permafrost degradation when large quantites of water were available. The amplitude of the involutions can be related to the depth of the permafrost table at that time. During the weichselian, two periods occurred in which this involution process could have been active |
format |
Article in Journal/Newspaper |
author |
VANDENBERGHE, JEF BROEK, PETER VAN DEN |
spellingShingle |
VANDENBERGHE, JEF BROEK, PETER VAN DEN Weichselian Convolution Phenomena and processes in fine sediments. |
author_facet |
VANDENBERGHE, JEF BROEK, PETER VAN DEN |
author_sort |
VANDENBERGHE, JEF |
title |
Weichselian Convolution Phenomena and processes in fine sediments. |
title_short |
Weichselian Convolution Phenomena and processes in fine sediments. |
title_full |
Weichselian Convolution Phenomena and processes in fine sediments. |
title_fullStr |
Weichselian Convolution Phenomena and processes in fine sediments. |
title_full_unstemmed |
Weichselian Convolution Phenomena and processes in fine sediments. |
title_sort |
weichselian convolution phenomena and processes in fine sediments. |
publisher |
Wiley |
publishDate |
1982 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1982.tb00539.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1982.tb00539.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1982.tb00539.x |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Boreas volume 11, issue 4, page 299-315 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1982.tb00539.x |
container_title |
Boreas |
container_volume |
11 |
container_issue |
4 |
container_start_page |
299 |
op_container_end_page |
315 |
_version_ |
1810471156450328576 |