Hutchinsonite
Hutchinsonite | |
---|---|
Hutchinsonite, from Quiruvilca Mine, Santiago de Chuco Province, Peru. Size: 4.5×4.4×2.2 cm | |
General | |
Category | Sulfide mineral |
Formula (repeating unit) | (Tl,Pb)2As5S9 |
Strunz classification | 2.HD.45 |
Crystal system | Orthorhombic |
Crystal class |
Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
Space group | Pbca |
Identification | |
Color | Red, pink, black |
Crystal habit | Acicular – cccurs as needle-like crystals |
Cleavage | {100} good |
Fracture | Very brittle fracture producing small, conchoidal fragments |
Mohs scale hardness | 1.5–2 |
Luster | Sub-metallic |
Streak | Red |
Diaphaneity | Subtranslucent to opaque |
Specific gravity | 4.6 |
Optical properties | biaxial (-) |
Refractive index |
nα = 3.078 nβ = 3.176 nγ = 3.188; 2V = 37° |
Birefringence | δ = 0.110 |
References | [1][2][3] |
Hutchinsonite is a sulfosalt mineral of thallium, arsenic and lead with formula (Tl,Pb)2As5S9. Hutchinsonite is a rare hydrothermal mineral.
It was first discovered in Binnental, Switzerland in 1904 and named after Cambridge mineralogist Arthur Hutchinson, F.R.S. (1866–1937).
See also
References
- ↑ Handbook of Mineralogy
- ↑ Hutchinsonite at Mindat.org
- ↑ Hutchinsonite at Webmineral
Further reading
- Prior, G. T. (1905). "A New Thallium Mineral". Nature. 71 (1849): 534. Bibcode:1905Natur..71Q.534P. doi:10.1038/071534b0.
Wikimedia Commons has media related to Hutchinsonite. |
This article is issued from Wikipedia - version of the 11/19/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.