Özet:

This study was conducted with the aim of revealing the stratigraphic characteristics of late Miyosen- Early Pliyosen old collapses in the west of Konya. The foundation of the review area is Paleozoic-Mesozoic old Basic rocks. On this basis, with angle incompatibility, Late Miyosen- Early Pliyosen comes to old Sille, Yalıtepe, Ulumuhsine, Little Mukhsine formations, Sulutas volcanoids, Early Pliyosen old Foot formations. The formation of the silk consists of a red colour conglomerate, a slurry and a slurry. The formation of the isole is made up of the beige, coffee-colored stromatolithic (LLH, SH, SS type). The formation of Ulumuhsine consists of beige, cream colored beige, cream colored beige, cream colored beige, cream, beige colored beige, cream, green cream colored marn, white, cream colored dolomite, coal black, grey colored beige, cream, beige colored four beige and banded beige and conglomerates. The formation of the smallmuhsine consists of volcanic breach, gun, gun and aglomerate, the member of the volcanic breach of Evlicoyuktepe, Mandalastepe gun member, Takkalıtepe gun member and Kanyakasıtepe aglomerate member. The Sulutaş volcanoes are composed of andezite and/or dasite. The formation of the Ulumuhsine and the formation of the Little Mouthsine, observed as a touch, is a red-colored conglomerate, red-colored and sharp-colored stumbling. All of these units are uncompatible with the angle of the Earth formation, which consists of a red, grey colour conglomerate, shell, beige, red colour and curved shell shell.

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