Ventifacts as palaeo‐wind indicators in southern Scandinavia
Abstract Systematic transect and grid surveys of ventifact presence/absence were made in order to assess palaeo‐ventifact abundance/distribution through Denmark and southern Sweden. The transects reveal a continuous ventifact distribution from western Denmark to south‐central Sweden giving evidence...
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crwiley:10.1002/ppp.3430060302 2024-06-02T08:08:16+00:00 Ventifacts as palaeo‐wind indicators in southern Scandinavia Schlyter, Peter 1995 http://dx.doi.org/10.1002/ppp.3430060302 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060302 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060302 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 6, issue 3, page 207-219 ISSN 1045-6740 1099-1530 journal-article 1995 crwiley https://doi.org/10.1002/ppp.3430060302 2024-05-03T10:57:09Z Abstract Systematic transect and grid surveys of ventifact presence/absence were made in order to assess palaeo‐ventifact abundance/distribution through Denmark and southern Sweden. The transects reveal a continuous ventifact distribution from western Denmark to south‐central Sweden giving evidence for the existence of significant palaeo‐wind action in extensive areas previously thought lacking in such evidence. Based on ice recession dates and vegetation development, ventifact formation is interpreted as having occurred mainly contemporaneously with the receeding Weichselian ice‐sheet. A grid survey in Scania, southern Sweden, demonstrates a continuous ventifact distribution irrespective of surface materials and topography. The ventifact occurrence outside areas with sandy soils indicates that suspended particles were effective abrading agents. Stable ventifacts confirm previous observations of easterly wind abrasion in Scania and exhibit an extremely small directional variability within, and between, sites. Ventifacts in southern Scandinavia are probably more indicative of transitory paraglacial conditions than periglacial conditions as such. Article in Journal/Newspaper Ice Sheet Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 6 3 207 219 |
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Open Polar |
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Wiley Online Library |
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English |
description |
Abstract Systematic transect and grid surveys of ventifact presence/absence were made in order to assess palaeo‐ventifact abundance/distribution through Denmark and southern Sweden. The transects reveal a continuous ventifact distribution from western Denmark to south‐central Sweden giving evidence for the existence of significant palaeo‐wind action in extensive areas previously thought lacking in such evidence. Based on ice recession dates and vegetation development, ventifact formation is interpreted as having occurred mainly contemporaneously with the receeding Weichselian ice‐sheet. A grid survey in Scania, southern Sweden, demonstrates a continuous ventifact distribution irrespective of surface materials and topography. The ventifact occurrence outside areas with sandy soils indicates that suspended particles were effective abrading agents. Stable ventifacts confirm previous observations of easterly wind abrasion in Scania and exhibit an extremely small directional variability within, and between, sites. Ventifacts in southern Scandinavia are probably more indicative of transitory paraglacial conditions than periglacial conditions as such. |
format |
Article in Journal/Newspaper |
author |
Schlyter, Peter |
spellingShingle |
Schlyter, Peter Ventifacts as palaeo‐wind indicators in southern Scandinavia |
author_facet |
Schlyter, Peter |
author_sort |
Schlyter, Peter |
title |
Ventifacts as palaeo‐wind indicators in southern Scandinavia |
title_short |
Ventifacts as palaeo‐wind indicators in southern Scandinavia |
title_full |
Ventifacts as palaeo‐wind indicators in southern Scandinavia |
title_fullStr |
Ventifacts as palaeo‐wind indicators in southern Scandinavia |
title_full_unstemmed |
Ventifacts as palaeo‐wind indicators in southern Scandinavia |
title_sort |
ventifacts as palaeo‐wind indicators in southern scandinavia |
publisher |
Wiley |
publishDate |
1995 |
url |
http://dx.doi.org/10.1002/ppp.3430060302 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060302 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060302 |
genre |
Ice Sheet Permafrost and Periglacial Processes |
genre_facet |
Ice Sheet Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 6, issue 3, page 207-219 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430060302 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
6 |
container_issue |
3 |
container_start_page |
207 |
op_container_end_page |
219 |
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1800753477992841216 |