Diana Cave, Romania
Speleothems: Crystals, crusts, earth masses (formed on a fragment of wood present in the cave)
Frequency: Extremely Rare
Other geologic settings: in evaporite deposits as a major component; in hydrothermal mineral deposit as an alteration mineral
Other occurrence: coatings, crusts (Ruatapu Cave,New Zealand; a cave in Big Bend, Texas, USA; Arnhem Cave, Namibia) powder (caves of Kahf al Mihnah, United Arab Emirates) helictites (up to 10 cm long and 0.3 cm wide)(Liquid Crystal Cave, Israel) small, white to blue crystals (Valea Rea Cave, Romania)
First description of cave occurrence: Diaconu, G. 1974. Quelques considérations sur la présence de l'anhydrite dans la grotte "Pestera Diana" (Baile Herculane-Roumanie). Travaux de l'Institute de Spéologie "Emile Racovitza" XIII: 191-194
First description of non-cave occurrence: Ludwig, C.F. 1804. A. G. Werners Mineral - System, Erste Klasse Erdige Fossilien, VI. Kalk - Geschlecht. Handbuch der Mineralogie nach A. G. Werner Volume 2 (Siegfried Lebrecht Crusius Leipzig): 209-212
Other cave locations & References: Ruatapu Cave, New Zealand - Cody, A.D. 1978. Ruatapu Cave. New Zealand Speleological Bulletin 6(108): 184-187 a cave from Big Bend National Park, Texas, USA: - Hill, C.A. 1979. Recent anhydrite and bassanite in Big Bend National Park caves. National Speleological Society Bulletin 42(4): 126-127 Arnhem Cave, Namibia; Stanton's Cave (Grand Canyon-USA) Valea Rea Cave, Romania - Onac, B.P., Bengeanu, M., Botez, M. & Zeh, J. 1995. Preliminary report on the mineralogy of Valea Rea Cave (Bihor Mountains, Romania). Theoretical and Applied Karstology 8: 75-79
Conservation and Protection: Anhydrite samples need to be preserved in dry environments.
Altitude: 154
Water: Yes (thermal)
Type of rock: Limestone/Marls
Age: Upper Jurassic - Lower Cretaceous
Cave climate type: Permanent bidirectional
Cave temperature (°C): 22
Cave humidity (%): 100
Group: Sulfates
Chemical formula: CaSO4
[According to the official IMA-CNMNC List of Mineral Names (http://nrmima.nrm.se/imalist.htm)]
- Orthorhombic
Prisms