| Reinerite | |
|---|---|
|   | |
| General | |
| Category | arsenite | 
| Formula | Zn3(AsO3)2 | 
| IMA symbol | Rnr [1] | 
| Strunz classification | 4.JA.10 | 
| Crystal system | Orthorhombic | 
| Crystal class | Dipyramidal (mmm)  H-M symbol: (2/m 2/m 2/m)  | 
| Space group | Pbam (no. 55) | 
| Unit cell | a = 6.092  Å, b = 14.407 Å  c = 7.811 Å; Z = 4 V = 685.55 a:b:c = 0.423 : 1 : 0.542  | 
| Identification | |
| Color | Sky blue, yellow green | 
| Crystal habit | Rough striated pseudohexagonal crystals | 
| Cleavage | Good on {110}, {011} and {111} | 
| Mohs scale hardness | 5 - 5.5 | 
| Luster | Vitreous to adamantine | 
| Diaphaneity | Transparent | 
| Specific gravity | 4.27 | 
| Optical properties | Biaxial (-) | 
| Refractive index | nα = 1.740 nβ = 1.790 nγ = 1.820 | 
| Birefringence | Maximum δ = 0.080 | 
| Other characteristics | Relief: very high | 
| References | [2] [3] [4] [5] | 
Reinerite is a rare arsenite (arsenate(III)) mineral with chemical formula Zn3(AsO3)2. [3] [4] It crystallizes in the orthorhombic crystal system.
Reinerite is most commonly found as a sky blue colored mineral, however, it may also be a light yellowish green color. Reinerite has a relative hardness of 5 to 5.5 on the Mohs Scale which is equivalent to that of a knife blade and or shard of glass. It has a density of 4.27 g/cm3, [2] and it exhibits a nonmetallic luster that may be described as glassy or vitreous. [6]
Reinerite develops in dolomite-hosted locations. It is known especially from Namibia, Africa, within the mines of Tsumeb. At the Tsumeb location, Reinerite develops within the polymetallic lead-zinc-copper deposit, 800 m (2,600 ft) below the surface, in the second oxidation zone. [5] It occurs in association with chalcocite, bornite, willemite, smithsonite, hydrozincite, hemimorphite, adamite, olivenite and gebhardite. [3]
Reinerite was first described in 1958 for an occurrence in the Tsumeb Mine, Tsumeb, Namibia and named for senior chemist Willy Reiner (1895–1965) of Tsumeb Corporation, who analyzed this mineral. [2] [4]