Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach
Abstract The slopes of Mt Ślęża, southwest Poland, are covered by debris covers that consist of gabbro blocks. Six classes of slope covers have been distinguished based on the concentration of blocks. A map of slope covers has been digitized and the following parameters have been defined: (i) concen...
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crwiley:10.1002/ppp.521 2024-06-02T08:13:10+00:00 Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach Żurawek, Roman Żyszkowski, Emil Górecki, Adam 2005 http://dx.doi.org/10.1002/ppp.521 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.521 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.521 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 16, issue 3, page 241-248 ISSN 1045-6740 1099-1530 journal-article 2005 crwiley https://doi.org/10.1002/ppp.521 2024-05-03T10:42:07Z Abstract The slopes of Mt Ślęża, southwest Poland, are covered by debris covers that consist of gabbro blocks. Six classes of slope covers have been distinguished based on the concentration of blocks. A map of slope covers has been digitized and the following parameters have been defined: (i) concentration of blocks on the slope, (ii) slope inclination, (iii) altitude, and (iv) aspect. The concentration of blocks has no correlation with either aspect or altitude. Instead, a dependence upon slope inclination is found. This suggests that slopewash explains the distribution of blocks on the present surface. Copyright © 2005 John Wiley & Sons, Ltd. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 16 3 241 248 |
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crwiley |
language |
English |
description |
Abstract The slopes of Mt Ślęża, southwest Poland, are covered by debris covers that consist of gabbro blocks. Six classes of slope covers have been distinguished based on the concentration of blocks. A map of slope covers has been digitized and the following parameters have been defined: (i) concentration of blocks on the slope, (ii) slope inclination, (iii) altitude, and (iv) aspect. The concentration of blocks has no correlation with either aspect or altitude. Instead, a dependence upon slope inclination is found. This suggests that slopewash explains the distribution of blocks on the present surface. Copyright © 2005 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Żurawek, Roman Żyszkowski, Emil Górecki, Adam |
spellingShingle |
Żurawek, Roman Żyszkowski, Emil Górecki, Adam Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
author_facet |
Żurawek, Roman Żyszkowski, Emil Górecki, Adam |
author_sort |
Żurawek, Roman |
title |
Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
title_short |
Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
title_full |
Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
title_fullStr |
Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
title_full_unstemmed |
Topographic control of periglacial slope covers, Ślęża Massif, southwest Poland: a statistical approach |
title_sort |
topographic control of periglacial slope covers, ślęża massif, southwest poland: a statistical approach |
publisher |
Wiley |
publishDate |
2005 |
url |
http://dx.doi.org/10.1002/ppp.521 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.521 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.521 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 16, issue 3, page 241-248 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.521 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
16 |
container_issue |
3 |
container_start_page |
241 |
op_container_end_page |
248 |
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1800759850197581824 |