Legrandite | |
---|---|
General | |
Category | Arsenate minerals |
Formula (repeating unit) | Zn2(AsO4)(OH)·(H2O) |
IMA symbol | Leg[1] |
Strunz classification | 8.DC.10 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/c |
Unit cell | a = 12.805(2), b = 7.933(1) c = 10.215(2) [Å]; β = 104.23°; Z = 8 |
Identification | |
Color | Bright yellow, wax-yellow, colorless |
Crystal habit | Crystalline, prismatic, typically in sprays or sheaflike aggregates |
Cleavage | Imperfect, poor one {100} |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 4.5-5 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 3.98–4.01 |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.675 - 1.702 nβ = 1.690 - 1.709 nγ = 1.735 - 1.740 |
Birefringence | δ = 0.060 |
Pleochroism | X = Y = Colorless to yellow Z = Yellow |
2V angle | Measured: 50° |
References | [2][3][4] |
Legrandite is a rare zinc arsenate mineral, Zn2(AsO4)(OH)·(H2O).
It is an uncommon secondary mineral in the oxidized zone of arsenic bearing zinc deposits and occurs rarely in granite pegmatite. Associated minerals include: adamite, paradamite, köttigite, scorodite, smithsonite, leiteite, renierite, pharmacosiderite, aurichalcite, siderite, goethite and pyrite.[2][3] It has been reported from Tsumeb, Namibia; the Ojuela mine in Durango, Mexico and at Sterling Hill, New Jersey, US.[2]
It was first described in 1934 for an occurrence in the Flor de Peña Mine, Nuevo León, Mexico and named after M. Legrand, a Belgian mining engineer .[3]
References
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- 1 2 3 Handbook of Mineralogy
- 1 2 3 Mindat.org
- ↑ Webmineral
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