Akademik Veri Yönetim Sistemi
MARMARA GEOGRAPHICAL REVIEW, sa.14, ss.29-60, 2006 (ESCI, TRDizin)
The Inegol Mountain is located in the Central Black Sea part of the Black Sea region. There are permanent and temporary settlements in this area and its administration is within the Amasya and Corum Province. Its geomorphologic properties are due to lithologic and tectonics factors. It forms a water boundary between the Kizilirmak and Yesilirmak plains. Formation of the high and low fields relative to one another were affected by different resistence and structures of rocks in this area. Lime stone and marble presence in this area caused the formation of karstik shapes. The physical appearance of the Inegol Mountain has been influenced by climate, lithologic properties and structure to a great deal as well as fluvyal periods. Inegol Mountain is surrounded by the depressions of Merzifon on the east, Osmancik on the west. The climate of this area is a typical continental climate with long winters wint snow falls, and short and cool summers.