Situated in the
eastern part of the Belianske Tatras over the Tatranska
Kotlina, in the National Nature Reserve Belianske Tatras,
in the territory of the Tatra National Park. It was
created in the Middle Triassic limestones by corrosion
and erosion waters from melting snow and ice or strong
precipitation. It reaches the length of 3,018 m. Sinter
„waterfalls", pagoda-like stalagmites and several sinter
pools are very attractive. Also other forms of sinter
filling are richly represented. Front parts of the cave
were known to gold miners as late as in the first half
of the 18th century. However, for long years to come,
the rest of the cave remained hidden to man’s eyes. It
was entered again in 1881. A part of the cave has been
open to the public as early as since 1882. Electric
lights were installed in 1896. At present, more than
1,000 m are accessible to the public.