Felsőbányaite
Felsőbányaite | |
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![]() Felsöbanyaite as white spherules. Roadcut near Sant Marti dels Castells (Lérida) Spain | |
General | |
Category | Sulfate mineral |
Formula (repeating unit) | Al4(SO4)(OH)10·4H2O |
Strunz classification | 7.DD.05 |
Crystal system | Monoclinic |
Crystal class | Sphenoidal (2) (same H-M symbol) |
Space group | P21 |
Unit cell | a = 13.026 Å, b = 10.015 Å, c = 11.115 Å; β = 104.34°; Z = 4 |
Identification | |
Color | White to pale yellow, pale brown |
Crystal habit | Globular masses, minute rhombic crystals |
Cleavage | Distinct to good on {010} and {100} |
Mohs scale hardness | 1.5 |
Luster | Vitreous, pearly on cleavage surfaces |
Diaphaneity | Semitransparent |
Specific gravity | 2.33 |
Optical properties | Biaxial (+) |
Refractive index | n = 1.515–1.540 |
References | [1][2] |
Felsőbányaite or basaluminite is a hydrated aluminium sulfate mineral with formula: Al4(SO4)(OH)10·4H2O. It is a rare white to pale yellow mineral which typically occurs as globular masses and incrustations or as minute rhombic crystals. It crystallizes in the monoclinic crystal system.[2][1]
It occurs as a weathering product under acidic conditions associated with pyrite or marcasite decomposition. Associated minerals include hydrobasaluminite, hydroargillite, meta-aluminite, allophane, gibbsite, gypsum and aragonite.[2]
Felsőbányaite was first described in 1853 for an occurrence in the Baia Sprie mine, Baia Sprie (Felsőbánya), Maramureș County, Romania, and named for the locality.[1] The mineral name basaluminite was used for an occurrence of the same mineral in England in 1948 and discredited by the International Mineralogical Association (IMA) in 2006.[3]