field of Turkey have been subject to different morphogenetic processes in geological past. It is observed that the units belong to different processes held together to constitute a basis in this issue when current existing geomorphological landscape is examined. In this regard, it may be mentioned that there is a variety of geomorphological elements dominated by the plüvyal morphogenetic process around Hatay. Different reflections of the plüvyal process, especially the post-Miocene, were found on the Kuseyr Plateau that builds up the work scope. Geomorphological units with different characteristics generated by changes in climate and tectonism proves that the morphogenetic process in this region works within a two-legged system. In this study, it has been explained which parameters are effective to changes on morphogenetic processes when they get involved in and what kind of factors control their geomorphological implications while examining how the units belong to different climageomorphological processes exist together depending on which variables on the Kuseyr Plateau. Thus, it is determined that processes with different characters controlled by tectonics different climatic conditions had been dominating formation of Kuseyr Plateau. Keywords: Morphogenesis, morphoclimate, Kuseyr Plateau, Hatay.
Alan : İlahiyat
Dergi Türü : Uluslararası
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