Situated in the
Vazecky Karst, at the meeting place of Kozie chrbty (Goat
Ranges) with the Liptovska Basin, at the western border
of Vazec. It was formed in the Middle Triassic
limestones by the former ponor waters of the White Vah
river. The length of the cave is 530 m. The cave spaces
are decorated mostly by stalactites, stalagmites and
sinter pools. It is an important finding-place of the
bones of speleal bear (Ursus spelaeus). The
entrance hall was long known to the local people. The
continuation of cave spaces was discovered in 1922. The
cave was provisionally open to the public in 1928. After
reconstruction in 1954, 235 m have been open to the
public.
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