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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Main Author: Kalińska Edyta
Format: Article
Language:English
Published: Sciendo 2006-12-01
Series:Miscellanea Geographica: Regional Studies on Development
Subjects:
Online Access:https://doi.org/10.2478/mgrsd-2006-0012
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spelling 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
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