Geography and Environment: It was formed within the Cretaceous aged; non-local crystallized limestones. It consists of three sections; which are as follows; continuously active section at the lower level; semi-active section at the middle level and fossil section at the upper level. In the active sections; there is an underground creek; maintaining its flow in summer or winter; which is indication of the fact that it is supplied in a well-balanced manner. Inside and outside cave; there are faulting; particularly fault breccias inside the cave. |