Geography and Environment: It is a fossil cave which was formed within the Eocene limestones over a pronounced fault line. It has three entrances; the main entrance is 20 m high from the valley; the second one is located at +13 m and the second one at +5.5 m in respect to the main entrance. Initially elongating in the northwest-southeast directions; it changed its direction in the mid where the second entrance is located toward north-south. At this point of change; a big depression hall of 50x60 m with a roof height of 30 m was developed. |