| Geography and Environment: On the contact zone of metaphormics overlaying the Menderes Massif with the Permian aged marbles; it was formed horizontally within the marbles. It has a small and narrow entrance. The section at the end of 130 m is at the same level with the entrance; which houses plenty of dripstone pools filled with water. Continuing to grow since the Pliocene epoch; all kinds of dripstone decorations can be seen inside the cave. It houses water throughout the year; and the underground creek disappears without resurging. |
