| Location: It can be reached by walking from the Yikik Quarter of the Kabaagac Village. The village is connected to the Fethiye-Kas motorway by an asphalted road. |
| Geography and Environment: It was formed within the Cretaceous aged conglomeratic limestones. The stones and rock pieces comprising the conglomerate were dissolved and collapsed into the cave. No travertine formation occurred. |
| Destruction Details: |
