Geography and Environment: It consists of three interconnected levels. The fossil level elongating in the west-east direction is an underground part of the Pliocene relief system. Depending on the easterly superficial drainage during Pliocene; the first section of the cave was formed below. The cave was lowered to the second level due to sinking into the channel of the Sofular Creek during the end of Pliocene Epoch. As sinking progressed; it resulted in the formation of the Dazdasi Sinkhole; Cayirköy Cave and the lower level of Sofular. |