New Geosite Candidates at the Western Termination of the Buyuk Menderes Graben and their Importance on Science Education

İnaner H., Sümer Ö., Akbulut M.

GEOHERITAGE, cilt.11, sa.4, ss.1291-1305, 2019 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 11 Sayı: 4
  • Basım Tarihi: 2019
  • Doi Numarası: 10.1007/s12371-019-00406-w
  • Dergi Adı: GEOHERITAGE
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.1291-1305
  • Anahtar Kelimeler: West Anatolian Extensional Province, Buyuk Menderes Graben, Volcanic rock suits, Normal fault, Marine fan delta, Geosite candidates, MESOZOIC COVER SERIES, PAN-AFRICAN BASEMENT, SW TURKEY, TECTONIC EVOLUTION, GEDIZ GRABEN, GRANITOID ROCKS, LYCIAN NAPPES, SOUTHWESTERN TURKEY, GEOLOGICAL HERITAGE, 2-STAGE EXTENSION
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

The Buyuk Menderes Graben (BMG) is one of the best-known and the largest geological structure of the West Anatolian Extensional Province. It includes two nature conservation parks and twelve cultural heritage sites within and in its vicinity. Four geologically distinct features/locations within and in the vicinity of the BMG have been previously enlisted as geosite candidates in the provisional Geological Heritage Inventory of Turkey compiled in 2002 by the Turkish Association for the Conservation of the Geological Heritage (JEMRKO): (1) the horst-graben structure of the Buyuk Menderes region itself, (2) the tafoni from the augen-gneiss from the east of Bafa Lake, (3) the zultanite crystals from the northeast of lbir Mountain, and (4) the tourmaline (dravite) crystals from the Camzal, Cine. In the current study, we are introducing additional three new geosite candidates at the western termination of the BMG with three different main geological subjects. The first one is the Yavansu Fault. Located 2 km south of the Kuadas village, it has a clearly exposed unique fault surface which is one of the best examples of structural indicators for the WAEP with respect to the normal faulting events. The second one is located in the Hisartepe Volcanics exposed between Kuadas and Soke, and consists of basaltic lava flows with remarkable prismatic cooling joints and a gorgeous feeder dome reaching up to 150 m height. Final suggestion is the Karina marine fan-delta complex located at the south-eastern border of the Dilek Peninsula National Park. This fan-delta complex is the largest one in the Western Anatolian scale and has remarkable paragon outcrops up to 20 m high between Doanbey and Karina Lagoon.