Abstract:

With its second high summit (October T. 3014 m), Akdağ is in a very high mass appearance compared to its surrounding area, located between the Eşen Ovası (60 m) east of the Apple Ovası (1100 m) and containing many heights over 2700 m. The main objective of the study is to study the ice shapes that occur in the Quaterner in the Mediterranean Mass and to date with OSL. In this study, geographical information systems and morphometric analyses, OSL datation method and sedimantological analyses were used. There have been several factors and processes in the geomorphological development of the body mass. At the beginning of these processes, the karst, ice, tectonic and fluvial come. The Pleistosen glaciations, which are effective in the midst mass, have been developed to a large extent in harmony with the carstical structure and have formed thick platonic glaciations in paleo-carstical depression at 2500 m and above. Three large, five ice valleys have been detected in the Mediterranean Mass. These ice valleys start with advanced circles and are covered with low-wing, broad-based and largely ground and side-more mores in accordance with paleocartistic depression at 2500 m levels, while after 2500 m levels, the valleys shrink and take the classic boat valleys shape and end with front mores at 2000 m levels. The OSL dates of the samples taken from the morena in the Medjugorje mass are 17-21 thousand years old, which is equal to the last ice period MIS 2.

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