Situated in the
Ochtinsky cryptokarst in the Revucka Highland, in the
massive of Hradok Hill, between Jelsava and Stitnik. It
was formed in a lens of Palaeozoic crystalline
limestones in the non-karst rocks (phyllites). A part
of the limestones was, in the Mesozoic Period in the
Upper Cretaceous, hydrothermically transformed into
ankerites and siderites. The seepage atmospheric water
seeping along the tectonic faults caused their
weathering and creation of ochres, that were later
flowed away. Overall length of the cave is 300 m. A rich
aragonite filling was formed under specific
hydrochemical and climatic conditions in closed
underground spaces. It occurs in kidney-shaped,
needle-shaped and spiral forms. The cave was discovered
in 1954 by chance, when driving a new geologic
exploratory gallery. It was open to the public in 1972
in the length of 230 m.