Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene
Vandenberghe, Jef, Bohncke, Sjoerd, Lammers, Wim & Zilverberg, Liesbeth 1987 03 01: Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene. Boreas , Vol. 16, pp. 55–67. Oslo. ISSN 0300–9483. The actual ar...
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crwiley:10.1111/j.1502-3885.1987.tb00754.x 2024-06-23T07:56:08+00:00 Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene VANDENBERGHE, JEF BOHNCKE, SJOERD LAMMERS, WIM ZILVERBERG, LIESBETH 1987 http://dx.doi.org/10.1111/j.1502-3885.1987.tb00754.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1987.tb00754.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1987.tb00754.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 16, issue 1, page 55-67 ISSN 0300-9483 1502-3885 journal-article 1987 crwiley https://doi.org/10.1111/j.1502-3885.1987.tb00754.x 2024-06-13T04:22:03Z Vandenberghe, Jef, Bohncke, Sjoerd, Lammers, Wim & Zilverberg, Liesbeth 1987 03 01: Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene. Boreas , Vol. 16, pp. 55–67. Oslo. ISSN 0300–9483. The actual area of the Mark valley is limited by the borders of an Early Weichselian erosion phase. The subsequent accumulation has resulted in the formation of a Weichselian Pleniglacial terrace which has been deeply dissected by Late Glacial erosion. The present alluvial plain is formed by Late Glacial and Holocene infilling. The maximum incision of the Late Glacial fluvial phase was reached slightly before 11,780 B.P. and involved locally dry conditions which have given rise to aeolian activity during this period (Older Dryas). On the deepest parts of the Pleniglacial terrace, a backswamp environment was established until the end of the Alleröd. At the beginning of the Younger Dryas the river invaded the terrace but shortly afterwards aeolian activity progressively increased. At the climax of the Younger Dryas, deep seasonal frost or local permafrost characterized the Mark valley. Article in Journal/Newspaper permafrost Wiley Online Library Boreas ENVELOPE(-3.933,-3.933,-71.300,-71.300) Lammers ENVELOPE(-66.333,-66.333,-68.617,-68.617) Boreas 16 1 55 67 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Vandenberghe, Jef, Bohncke, Sjoerd, Lammers, Wim & Zilverberg, Liesbeth 1987 03 01: Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene. Boreas , Vol. 16, pp. 55–67. Oslo. ISSN 0300–9483. The actual area of the Mark valley is limited by the borders of an Early Weichselian erosion phase. The subsequent accumulation has resulted in the formation of a Weichselian Pleniglacial terrace which has been deeply dissected by Late Glacial erosion. The present alluvial plain is formed by Late Glacial and Holocene infilling. The maximum incision of the Late Glacial fluvial phase was reached slightly before 11,780 B.P. and involved locally dry conditions which have given rise to aeolian activity during this period (Older Dryas). On the deepest parts of the Pleniglacial terrace, a backswamp environment was established until the end of the Alleröd. At the beginning of the Younger Dryas the river invaded the terrace but shortly afterwards aeolian activity progressively increased. At the climax of the Younger Dryas, deep seasonal frost or local permafrost characterized the Mark valley. |
format |
Article in Journal/Newspaper |
author |
VANDENBERGHE, JEF BOHNCKE, SJOERD LAMMERS, WIM ZILVERBERG, LIESBETH |
spellingShingle |
VANDENBERGHE, JEF BOHNCKE, SJOERD LAMMERS, WIM ZILVERBERG, LIESBETH Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
author_facet |
VANDENBERGHE, JEF BOHNCKE, SJOERD LAMMERS, WIM ZILVERBERG, LIESBETH |
author_sort |
VANDENBERGHE, JEF |
title |
Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
title_short |
Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
title_full |
Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
title_fullStr |
Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
title_full_unstemmed |
Geomorphology and palaeoecology of the Mark valley (southern Netherlands): geomorphological valley development during the Weichselian and Holocene |
title_sort |
geomorphology and palaeoecology of the mark valley (southern netherlands): geomorphological valley development during the weichselian and holocene |
publisher |
Wiley |
publishDate |
1987 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1987.tb00754.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1987.tb00754.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1987.tb00754.x |
long_lat |
ENVELOPE(-3.933,-3.933,-71.300,-71.300) ENVELOPE(-66.333,-66.333,-68.617,-68.617) |
geographic |
Boreas Lammers |
geographic_facet |
Boreas Lammers |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Boreas volume 16, issue 1, page 55-67 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1987.tb00754.x |
container_title |
Boreas |
container_volume |
16 |
container_issue |
1 |
container_start_page |
55 |
op_container_end_page |
67 |
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1802649022812389376 |