Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/58641
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dc.contributor.authorTopal, Savas-
dc.contributor.authorIrfan, Mohammad-
dc.date.accessioned2025-01-22T17:14:05Z-
dc.date.available2025-01-22T17:14:05Z-
dc.date.issued2025-
dc.identifier.issn1672-6316-
dc.identifier.issn1993-0321-
dc.identifier.urihttps://doi.org/10.1007/s11629-024-9132-8-
dc.identifier.urihttps://hdl.handle.net/11499/58641-
dc.description.abstractDrainage divide migration refers to the shifting boundaries between adjacent drainage basins over time, driven by processes such as tectonic uplift, differential erosion, stream capture, and lithological variations. This phenomenon has a significant impact on water flow patterns and basin extents, serving as an indicator of the landscape's response to active tectonic forces. One of the key drivers of divide migration is asymmetric uplift, which causes divides to shift from areas of lower uplift to regions experiencing higher uplift. Drainage divides are inherently dynamic, evolving over time as drainage networks develop and adjust to changing conditions. This study focuses on the migration of the main drainage divide along Kar & imath;ncal & imath;da & gbreve;, located between Bozdo & gbreve;an and Karacasu. It employs geomorphic analyses using metrics such as the normalized steepness index (ksn), Chi (chi), and Gilbert metrics. The main divide is categorized into four segments (D1-D4), with the Karacasu Fault, situated along the mountain's north-eastern boundary, identified as the primary factor influencing divide dynamics. Secondary factors include the relatively low elevation of Kar & imath;ncal & imath;da & gbreve;, uniform lithology, and consistent rainfall patterns across the region. The results indicate that the main divide is currently stable, suggesting a balance between uplift and erosion. However, higher chi values in the D4 segment suggest that future erosion may dominate, potentially causing the divide to migrate toward the Bozdo & gbreve;an Basin. These findings highlight the dynamic nature of drainage divides and the complex interplay of tectonic, erosional, and lithological processes that shape their evolution. Continued monitoring and advanced geomorphic analysis are essential for understanding the long-term stability of the divide and its response to future tectonic activity and erosional modifications.en_US
dc.language.isoenen_US
dc.publisherScience Pressen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectDrainage Divide Migrationen_US
dc.subjectGilbert Metricsen_US
dc.subjectKar & Imathen_US
dc.subjectNcal & Imathen_US
dc.subjectDa & Gbreveen_US
dc.subjectKaracasu Faulten_US
dc.titleNormal Faulting and Its Role in the Drainage Divide Migration in the Karıncalıdağ Region, Menderes Massif, Western Türkiyeen_US
dc.typeArticleen_US
dc.departmentPamukkale Universityen_US
dc.identifier.doi10.1007/s11629-024-9132-8-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorscopusid56575514000-
dc.authorscopusid58698016800-
dc.authorwosidTopal, Savaş/I-1233-2012-
dc.identifier.scopus2-s2.0-85214360131-
dc.identifier.wosWOS:001390960100001-
dc.identifier.scopusqualityQ3-
dc.description.woscitationindexScience Citation Index Expanded-
dc.identifier.wosqualityQ3-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.openairetypeArticle-
item.fulltextNo Fulltext-
item.cerifentitytypePublications-
item.grantfulltextnone-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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