Ochtinská Aragonite Cave
Ochtinská Aragonite Cave (Slovak: Ochtinská aragonitová jaskyňa, Hungarian: Martonházi-aragonitbarlang) is a unique aragonite cave situated in southern Slovakia, near Rožňava. Although only 300 m long, it is famous for its rare aragonite formations.[2]
Ochtinská Aragonite Cave | |
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Slovak: Ochtinská aragonitová jaskyňa | |
White aragonite forms the cave's rare attractions | |
Location | Slovak Karst, Slovakia |
Length | 300 m |
Height variation | 30 m |
Elevation | 642 m |
Discovery | 1954 |
Geology | aragonite |
Visitors | 26,591 (2009) [1] |
Description
There are only three aragonite caves discovered in the world so far.
In the so-called Milky Way Hall, the main attraction of the cave, white branches and clusters of aragonite shine like stars in the Milky Way. The cave was discovered by Martin Cangár and Jiri Prosek in 1954 and opened to the public in 1972. Along with other caves of the Slovak Karst, it is included in the UNESCO World Heritage list as a component of Caves of Aggtelek Karst and Slovak Karst site.[3]
gollark: Bell's theorem rules out "local hidden-variables" interpretations of quantum physics, meaning that quantum mechanics cannot, assuming some assumptions, be doing this by storing some extra secret metadata with particles.
gollark: As you will know in time, quantum QM mechanics has "Bell's theorem". This describes some correlations between measurements of entangled particles which QM predicts correctly (based on empirical tests) and classical physics doesn't.
gollark: What? No. That would be stupid.
gollark: Yes.
gollark: Determinism is outdated. I'm a *super*determinist.
See also
Gallery
- Aragonite inside the cave
References
- "Archived copy". Archived from the original on 2013-04-22. Retrieved 2010-11-20.CS1 maint: archived copy as title (link)
- Lucinda Mallows, Lucy Mallows (2007). Slovakia: The Bradt Travel Guide. Bradt Travel Guides. p. 6. ISBN 1-84162-188-9.
- Mallows, Lucy (2007). "Ochtínská aragonitová jaskyňa (cave)". Slovakia. pp. 293–4. ISBN 978-1-84162-188-3.
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