Landslide susceptibility mapping of SE Serbia using GIS
Landslides represent a great problem in Serbia. According to current estimates 30-35 % of Serbia is affected by landslides. In this paper a landslide susceptibility analysis is done for SE Serbia. Study area covers 1507 km2. Relief is hilly or mountainous and characterized by high altitude...
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Faculty of Mining and Geology, Belgrade
2019-01-01
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Online Access: | http://www.doiserbia.nb.rs/img/doi/0350-0608/2019/0350-06081902105D.pdf |
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doaj-763dd1a5445846f4a0d5dbdb399c12b42020-11-25T02:34:55ZengFaculty of Mining and Geology, BelgradeGeološki Anali Balkanskoga Poluostrva0350-06082406-07472019-01-0180210511610.2298/GABP1902105D0350-06081902105DLandslide susceptibility mapping of SE Serbia using GISĐokanović Sonja0Geological survey of Serbia, Belgrade, SerbiaLandslides represent a great problem in Serbia. According to current estimates 30-35 % of Serbia is affected by landslides. In this paper a landslide susceptibility analysis is done for SE Serbia. Study area covers 1507 km2. Relief is hilly or mountainous and characterized by high altitude differences. Analysis is done by geographic information system (GIS) and evaluation by analytic hierarchy process (AHP). For susceptibility assessment are used four factors: lithology, slope angle, distance to rivers and distance to faults. The most landslides are formed on slope steepness less than 30°. There is four classes of susceptibility in study area. Zone of very high susceptibility make 63.9 % of the study area. Zone of high susceptibility covers 15.7 % of the study area. The moderate class occupies 37.4% and zone classified as having low susceptibility accounts for 10 % of study area. Final landslide susceptibility map of SE Serbia is satisfactory.http://www.doiserbia.nb.rs/img/doi/0350-0608/2019/0350-06081902105D.pdflandslidesusceptibilityahplithologyslope |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Đokanović Sonja |
spellingShingle |
Đokanović Sonja Landslide susceptibility mapping of SE Serbia using GIS Geološki Anali Balkanskoga Poluostrva landslide susceptibility ahp lithology slope |
author_facet |
Đokanović Sonja |
author_sort |
Đokanović Sonja |
title |
Landslide susceptibility mapping of SE Serbia using GIS |
title_short |
Landslide susceptibility mapping of SE Serbia using GIS |
title_full |
Landslide susceptibility mapping of SE Serbia using GIS |
title_fullStr |
Landslide susceptibility mapping of SE Serbia using GIS |
title_full_unstemmed |
Landslide susceptibility mapping of SE Serbia using GIS |
title_sort |
landslide susceptibility mapping of se serbia using gis |
publisher |
Faculty of Mining and Geology, Belgrade |
series |
Geološki Anali Balkanskoga Poluostrva |
issn |
0350-0608 2406-0747 |
publishDate |
2019-01-01 |
description |
Landslides represent a great problem in Serbia. According to current
estimates 30-35 % of Serbia is affected by landslides. In this paper a
landslide susceptibility analysis is done for SE Serbia. Study area covers
1507 km2. Relief is hilly or mountainous and characterized by high altitude
differences. Analysis is done by geographic information system (GIS) and
evaluation by analytic hierarchy process (AHP). For susceptibility
assessment are used four factors: lithology, slope angle, distance to rivers
and distance to faults. The most landslides are formed on slope steepness
less than 30°. There is four classes of susceptibility in study area. Zone
of very high susceptibility make 63.9 % of the study area. Zone of high
susceptibility covers 15.7 % of the study area. The moderate class occupies
37.4% and zone classified as having low susceptibility accounts for 10 % of
study area. Final landslide susceptibility map of SE Serbia is satisfactory. |
topic |
landslide susceptibility ahp lithology slope |
url |
http://www.doiserbia.nb.rs/img/doi/0350-0608/2019/0350-06081902105D.pdf |
work_keys_str_mv |
AT đokanovicsonja landslidesusceptibilitymappingofseserbiausinggis |
_version_ |
1724806510280704000 |