Geological and Geomorphological Analysis of the Ancient Erenkoy and Guzelyali Landslides in the Canakkale District, NW Turkey

Basit Öğe Kaydı
dc.contributor.authorPerincek, Dogan
dc.date.accessioned2025-01-27T20:47:39Z
dc.date.available2025-01-27T20:47:39Z
dc.date.issued2018
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe study was able to describe the ancient landslide debris around Guzelyali Village. Also, the remains of horrendous ancient landslides have been discovered in northeast of Erenkoy Village in Canakkale. In this frame, aim of the study is to determine the preparatory and triggering factors that form the landslides by analyzing the occurrence and development mechanisms of these landslides with the geological and geomorphologic methods. The evidence for the ancient landslide triggered by 1875 Erenkoy-Canakkale Earthquake presented in this paper, which is located near Erenkoy. Ancient landslide complex around Erenkoy-Guzelyali area has the distinction of having one of the largest, landslides in Canakkale. The total area of the ancient landslides is approximately 3.75 square kilometers in size. Historical landslides near Erenkoy have been noticed by land features bearing two hallmark characteristics. These are: a jumbled assortment of rocks at the base of a slope, and a cuplike or sharp-straight topography cut out of the hills where the slide might have come from. Post 1875 erosion activity have partially erased much of the evidence of landslide. It was assumed that landslide deposits near Guzelyali Village were produced by multiple landslide events. Probably some of the slides, originated by earthquakes consisting of many events, likely several -undred years between them. Mentioned landslide debris was recently moved again as creep-type landslides. Ancient landslide debris offers danger signs for northeastern Guzelyali housing developments. Ancient Guzelyali's landslide debris and related landslide is older than Erenkoy's landslide.
dc.identifier.doi10.25288/tjb.458432
dc.identifier.endpage267
dc.identifier.issn1016-9164
dc.identifier.issue3
dc.identifier.startpage241
dc.identifier.urihttps://doi.org/10.25288/tjb.458432
dc.identifier.urihttps://hdl.handle.net/20.500.12428/24997
dc.identifier.volume61
dc.identifier.wosWOS:000455157100001
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.language.isotr
dc.publisherTmmob Jeoloji Muhendisleri Odasi
dc.relation.ispartofTurkiye Jeoloji Bulteni-Geological Bulletin of Turkey
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WoS_20250125
dc.subjectCanakkale
dc.subjectErenkoy
dc.subjectGuzelyali
dc.subjectlandslide
dc.subjectcreep
dc.subjectrotational slide
dc.titleGeological and Geomorphological Analysis of the Ancient Erenkoy and Guzelyali Landslides in the Canakkale District, NW Turkey
dc.typeArticle

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