| Location: It is located near the Durabeyler Village; approximately 14 km north of Dursunbey. It lies on the left bank of the Tasovasi Creek. A road leads near to the cave from the Dursunbey District. |
| Geography and Environment: It was formed along a pronounced fault line within the Permian marbles. Formed as resurgence; today it is completely a fossil cave. It is composed of two interconnected branches; and it is adorned with stalactites; stalagmites; columns; draperies and wall dripstones. It is dry in all seasons. |
| Destruction Details: |
