Fingerite
Fingerite is a copper vanadate mineral with formula: β-Cu2V2O5. It was discovered as triclinic crystals occurring as volcanic sublimates around fumaroles in the crater of the Izalco Volcano, El Salvador.
Fingerite | |
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General | |
Category | Vanadate mineral |
Formula (repeating unit) | β-Cu2V2O5 |
Strunz classification | 8.BB.80 |
Crystal system | Triclinic |
Crystal class | Pinacoidal (1) H-M symbol: (1) |
Space group | P1 |
Unit cell | a = 8.16, b = 8.27 c = 8.04 [Å]; α = 107.14° β = 91.39°, γ = 106.44°; Z = 1 |
Identification | |
Color | Black; medium gray in reflected light |
Crystal habit | Subhedral or anhedral; equant or platelike; up to 150 μm |
Cleavage | None |
Luster | Metallic |
Streak | Dark reddish brown |
Diaphaneity | Opaque |
Density | 4.78 |
Optical properties | Biaxial |
References | [1][2][3] |
Associated minerals include thenardite, euchlorine, stoiberite, shcherbinaite, ziesite, bannermanite, chalcocyanite and chalcanthite.[1] The mineral also dissolves in water.
Fingerite is named for Dr. Larry W. Finger (b. 1940) of the Geophysical Laboratory, Carnegie Institution of Washington.
References
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