The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny)
The vicinity of Kazimierz Dolny is characterised by the occurrence of large denivelations and thick loess covers. Due to that, as well as to the characteristic properties of loess and frequent occurrences of torrential rains, the region is marked by numerous dissections by valleys. Not without impor...
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2006-12-01
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Series: | Miscellanea Geographica: Regional Studies on Development |
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Online Access: | https://doi.org/10.2478/mgrsd-2006-0012 |
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doaj-4d29272803134b3681b4f2be9ecf0af72021-09-06T19:22:31ZengSciendoMiscellanea Geographica: Regional Studies on Development2084-61182006-12-0112110311010.2478/mgrsd-2006-0012The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny)Kalińska Edyta0Faculty of GeologyThe vicinity of Kazimierz Dolny is characterised by the occurrence of large denivelations and thick loess covers. Due to that, as well as to the characteristic properties of loess and frequent occurrences of torrential rains, the region is marked by numerous dissections by valleys. Not without importance is agriculture, whose intensification brought about the creation of new relief forms. Gully erosion is a serious threat for the inhabitants of the region; on the other hand, it is impossible to eliminate it. For that reason it is necessary to use modern anti-erosion measures.https://doi.org/10.2478/mgrsd-2006-0012denivelationsthick loess coversvalleydownflowsuffosiontorrential rainssiltinganti-erosion measures |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Kalińska Edyta |
spellingShingle |
Kalińska Edyta The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) Miscellanea Geographica: Regional Studies on Development denivelations thick loess covers valley downflow suffosion torrential rains silting anti-erosion measures |
author_facet |
Kalińska Edyta |
author_sort |
Kalińska Edyta |
title |
The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) |
title_short |
The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) |
title_full |
The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) |
title_fullStr |
The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) |
title_full_unstemmed |
The Role of Morphogenetic and Anthropogenic Processes in The Development of Gullies and Methods of Their Prevention (On The Example of The Vicinity of Kazimierz Dolny) |
title_sort |
role of morphogenetic and anthropogenic processes in the development of gullies and methods of their prevention (on the example of the vicinity of kazimierz dolny) |
publisher |
Sciendo |
series |
Miscellanea Geographica: Regional Studies on Development |
issn |
2084-6118 |
publishDate |
2006-12-01 |
description |
The vicinity of Kazimierz Dolny is characterised by the occurrence of large denivelations and thick loess covers. Due to that, as well as to the characteristic properties of loess and frequent occurrences of torrential rains, the region is marked by numerous dissections by valleys. Not without importance is agriculture, whose intensification brought about the creation of new relief forms. Gully erosion is a serious threat for the inhabitants of the region; on the other hand, it is impossible to eliminate it. For that reason it is necessary to use modern anti-erosion measures. |
topic |
denivelations thick loess covers valley downflow suffosion torrential rains silting anti-erosion measures |
url |
https://doi.org/10.2478/mgrsd-2006-0012 |
work_keys_str_mv |
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