Abstract
The Study area is located in the Mediterranean region and its sub region Adana. Its far of the Kozan district is 50 km Northeast direction. Gezit Polje is (UTM: 251442 E, 4179840 N) 37°43'56"N latitude and 36°10'46"E longitude in terms of Geographical Coordinate System. Gezit Polje which extents NE-SW direction demonstrates parallelism in respect of direction Middle Tours. It is 1986 m. from sea level. The Polje has been shaped with carstification, erosion and tectonic movements in the Upper Miocene Conglomerates. Poljes have been shaped with carstification together tectonic movements/lines. Gezit Polje has been occurred with faults which are formed between Misis and Göksun east part of Gezit Mountain. West part has been shaped with Göksu Fault. This polje is different more than other poljes because it has formed Upper Miocene Conglomerate rocks. This Formation covers more than other old formations in terms of angular incongruous. This is because Carstification landforms and term of c
Keywords
Poljes, Gezit Polje, Carstification of Miocene Conglomerates.
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