Tuesday, July 21, 2009

Prehnite

Prehnite

Prehnite

Prehnite, Epidote
General
CategorySilicate mineral
Chemical formulaCa2Al(AlSi3O10)(OH)2
Identification
ColorColorless to gray to yellow, yellow-green or white
Crystal habitGlobular, reniform to stalactitic
Crystal systemOrthorhombic - Pyramidal
CleavageDistinct on [001]
FractureBrittle
Mohs Scalehardness6 - 6.5
LusterVitreous - pearly
Specific gravity2.8 - 2.95
Optical propertiesBiaxial (+)
Refractive indexnα = 1.611 - 1.632 nβ = 1.615 - 1.642 nγ = 1.632 - 1.665
Birefringenceδ = 0.021 - 0.033
References[1][2][3]

Prehnite is a phyllosilicate of calcium and aluminium with the formula: Ca2Al(AlSi3O10)(OH)2. Limited Fe3+ substitutes for aluminium in the structure. Prehnite crystallizes in theorthorhombic crystal system. It is brittle with an uneven fracture and a vitreous to pearly lustre. Its hardness is 6-6.5, its specific gravity is 2.80-2.90 and its color varies from light green to blue or white. It is translucent.

Though not a zeolite, it is found associated with them and with datolite, calcite, etc. in veins and cavities of basaltic rocks, sometimes in granites, syenites, or gneisses. It is an indicator mineral of the prehnite-pumpellyite metamorphic facies. It was first described in 1789 for an occurrence in Haslach, Harzburg and Oberstein, Germany, and named for Colonel Hendrik Von Prehn (1733-1785), an early Dutch governor of the Cape of Good Hope colony.[1]


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