| Location: It lies to 5 km of the Mürüvetler Village; 5 km southeast of Manyas. Developed on the upper right slope of the Karakuza Creek which drains into the Manyas Lake and flows in deeply buried valleys; it can be reached by walking from the bed of creek. |
| Geography and Environment: It was formed within the Permian aged crystallized limestones or marbles. It is a spring type of fossil cave. It is adorned with wall dripstones and columns at some sections. Generally; it is dry in all seasons. |
| Destruction Details: |
