Arnhem Cave, Namibia - mineral species not approved by IMA
First description of cave occurrence: Martini, J. E. 1994. Two new minerals originated from bat guano combustion in Arnhem Cave, Namibia. Bulletin of the South African Speleological Association 33: 66-69
First description of non-cave occurrence: -
Other cave locations & References: Hibashi Cave. Saudi Arabia - Pint, J.J., Al-Shanti, M.A., Al-Juaid, A.J., Al-Amoudi, S.A. & Forti, P. 2005. Ghar al Hibashi Harrat Nawasif/Al Buqum, Kingdom of Saudi Arabia. Saudi Geological Survey Open-File Report SGS-OF-2004-12: 68pp (http://www.i-pi.com/~ingham/saudicaves/hib-4-12.pdf)
Longitude: 18°5'47''E
Length: 4500
Water: No
Type of rock: Dolomite
Age: Precambrian
Cave temperature (°C): 25
Chemical formula: K4Mg2(P2O7)·5H2O
[According to the official IMA-CNMNC List of Mineral Names (http://nrmima.nrm.se/imalist.htm)]
Deposition and stability: It is not a a direct product of guano combustion, but is the likely formed by secondary hydration of a primary anhydrous K-Mg pyrophosphate generated at high temperature. No relic of such a pyrophosphate has been identified in the white slag.
Color: White
Luster: Pearly
Hardness: Low (not measured)
Cleavage: Extinction if parallel to the cleavage {001}
Electron microprobe, gas chromatography, optical properties
Cell parameter c (Å): 16.75
Crystal size: 1 to 50 microns