Landslide susceptibility mapping using Bayesian approach in the Sultan Mountains (AkAYehir, Turkey)

dc.contributor.authorOzdemir, Adnan
dc.date.accessioned2020-03-26T18:15:08Z
dc.date.available2020-03-26T18:15:08Z
dc.date.issued2011
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractLandslides cause heavy damage to property and infrastructure, in addition to being responsible for the loss of human lives in many parts of the Turkey. The paper presents GIS-based spatial data analysis for landslide susceptibility mapping in the regions of the Sultan Mountains, West of AkAYehir, and central part of Turkey. Landslides occur frequently in the area and seriously affect local living conditions. Therefore, spatial analysis of landslide susceptibility in the Sultan Mountains is important. The relationships between landslide distributions with the 19 landslide affecting parameters were analysed using a Bayesian model. In the study area, 90 landslides were observed. The landslides were randomly subdivided into 80 training landslides and 10 test landslides. A landslide susceptibility map was produced by using the training landslides. The test landslides were used in the accuracy control of the produced landslide susceptibility map. Approximately 9% of the study area was classified as high susceptibility zone. Medium, low and very low susceptibility zones covered 8, 23 and 60% of the study area, respectively. Most of the locations of the observed landslides actually fall into moderate (17.78%) and high (77.78. %) susceptibility zones of the produced landslide susceptibility map. This validates the applicability of proposed methods, approaches and the classification scheme. The high susceptibility zone is along both sides of the AkAYehir Fault and at the north-eastern slope of the Sultan Mountains. It was determined that the surface area of the Harlak and Deresenek formations, which have attained lithological characteristics of clayey limestone with a broken and separated base, and where area landslides occur, possesses an elevation of 1,100-1,600 m, a slope gradient of 25A degrees-35A degrees and a slope aspect of 22.5A degrees-157.5A degrees facing slopes.en_US
dc.identifier.doi10.1007/s11069-011-9853-1en_US
dc.identifier.endpage1607en_US
dc.identifier.issn0921-030Xen_US
dc.identifier.issn1573-0840en_US
dc.identifier.issue3en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage1573en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s11069-011-9853-1
dc.identifier.urihttps://hdl.handle.net/20.500.12395/26613
dc.identifier.volume59en_US
dc.identifier.wosWOS:000296475400019en_US
dc.identifier.wosqualityQ2en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSPRINGERen_US
dc.relation.ispartofNATURAL HAZARDSen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectLandslideen_US
dc.subjectSusceptibilityen_US
dc.subjectGISen_US
dc.subjectWeights of evidenceen_US
dc.subjectThe Sultan Mountainsen_US
dc.subjectTurkeyen_US
dc.titleLandslide susceptibility mapping using Bayesian approach in the Sultan Mountains (AkAYehir, Turkey)en_US
dc.typeArticleen_US

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