| Location: It can be reached from Gümüshane by car passing through the quarters of Yuvanet-Sismanli-Arsa-Kabanbasi or by a 1 hour walking through the pathway leading to the Kabanbasi Quarter from the Eskibaglar Quarter. |
| Geography and Environment: It is a spring type of fossil cave; which was developed horizontally. It was formed within the highly fractured and jointed Malm Lower Cretaceous limestones. The walls of the cave; which becomes narrower onward; are partly adorned with dripstone decorations. The floor is covered sometimes by rocky blocks and sometimes by earth and guano. It is dry in all seasons |
| Destruction Details: |
