Situated on the Horný vrch Plateau, westerly from the upper part of the Zádielska Gorge. Typical, gravitationally widened crevasse cave reaches the length of 100 m and depth of 25 m. The roof is closed by collapsed boulders. It is formed in the Mesozoic Middle Triassic pale Wetterstein limestones of the Silica Nappe.
The cave has pea flowstone decoration in some places. There are smaller dripstones and layers of ice fill in the western part of the cave. The ice partially melts in summer months, yet it persists all year round.
Invertebrates are represented by multipede Hylebainosoma tatranum, which is Western Carpathian endemic species. Harvestman Ischyropsalis manicata is a representative of troglophilic spiders on cave walls.
Dear visitors, the Domica cave will be closed on 22nd of May 2025 due to operational reasons. We apologize for any inconvenience.
Vážení návštevníci, jaskyňa Domica bude dňa 22.5.2025 z prevádzkových dôvodov po celý deň pre verejnosť zatvorená. Ďakujeme za pochopenie.
Dear visitors, we would like to inform you that due to the technical conditions of payment terminals, there may be situations when card payment will not be possible. For this reason, we recommend that you have an adequate amount of cash available if you want to be sure that you will be able to visit the cave. Thank you for understanding.