The Quaternary landforms of the Buyuk Menderes Graben System: the southern Menderes Massif, western Anatolia, Turkey

Ozpolat E., Yıldırım C., Görüm T.

JOURNAL OF MAPS, cilt.16, sa.2, ss.405-419, 2020 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 16 Sayı: 2
  • Basım Tarihi: 2020
  • Doi Numarası: 10.1080/17445647.2020.1764874
  • Dergi Adı: JOURNAL OF MAPS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Social Sciences Citation Index (SSCI), Scopus, Academic Search Premier, Directory of Open Access Journals
  • Sayfa Sayıları: ss.405-419
  • Anahtar Kelimeler: Extensional landscape, alluvial fan, river terrace, Red Relief Image Map, western Anatolia, Menderes Massif, ALLUVIAL FANS, TECTONIC GEOMORPHOLOGY, AXIAL RIVERS, EVOLUTION, EXTENSION, GEDIZ, SEDIMENTATION, TOPOGRAPHY, TERRACES, KARACASU
  • İstanbul Teknik Üniversitesi Adresli: Evet

Özet

We present the first detailed Quaternary landform map of the Buyuk Menderes Graben System, located in western Turkey which is one of the most active extensional domains in the world. The main map was produced with a combination of TanDEM-X (12.5 m resolution), Red Relief Image Map, unmanned aerial vehicle, Google Earth images, and multiple fieldworks. The main map is presented at a scale of 1:160,000 although landforms were mapped at a scale of 1:15,000. The ten Quaternary landforms were defined considering their surface morphology and depositional environment. The alluvial fans, river terraces, and floodplains are the most common landforms. The spatial pattern of the alluvial fans and river terraces showed the variable rates of tectonics and surface processes along the strike of the graben system. The distribution of the meander cut-offs and paleo-shorelines imply that Buyuk Menderes Graben System is vulnerable to geohazards like flash-flood sedimentation and flood events.