Cervantite
Cervantite | |
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Microscopic cervantite crystals from Slovakia (3 mm field of view)
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General | |
Category | Oxide mineral |
Formula (repeating unit) |
Sb3+Sb5+O4 |
Strunz classification | 04.DE.30 |
Crystal symmetry | Orthorhombic pyramidal H-M symbol: (mm2) Space group: Pbn21 |
Unit cell | a = 5.43 Å, b = 4.81 Å, c = 11.76 Å; Z = 4 |
Identification | |
Color | Yellow to nearly white |
Crystal habit | Microscopic acicular crystals; massive |
Crystal system | Orthorhombic |
Cleavage | Excellent on {001}, distinct on {100} |
Fracture | Conchoidal |
Mohs scale hardness | 4–5 |
Luster | Greasy, pearly, earthy |
Streak | Pale yellow to white |
Diaphaneity | Semitransparent |
Specific gravity | 6.5 |
Optical properties | Biaxial |
Refractive index | nα = 2.000 nγ = 2.100 |
Birefringence | δ = 0.100 |
Dispersion | relatively weak |
References | [1][2][3] |
Cervantite is an antimony oxide mineral with formula Sb3+Sb5+O4 (antimony tetroxide).
It was first described in 1850 for an occurrence in Cervantes, Sierra de Ancares, Lugo, Galicia, Spain, and named for the locality.[2] The mineral was questioned and disapproved, but re-approved and verified in 1962 based on material from the Zajaca-Stolice district, Brasina, Serbia.[1] It occurs as a secondary alteration product of antimony bearing minerals, mainly stibnite.[1]
References
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