Volborthite

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Volborthite
Volborthite-263832.jpg
Volborthite crystals from the Ridenaur Mine, Prospect Canyon District, Coconino County, Arizona (size: 5.8 x 4.5 x 4.2 cm)
General
Category Polyvanadate minerals
Formula
(repeating unit)
Cu3V2O7(OH)2·2H2O
Strunz classification 08.FD.05
Crystal symmetry Monoclinic prismatic
H-M symbol (2/m)
Space group: C 2/m
Unit cell a = 10.610(2) Å, b = 5.866(1) Å, c = 7.208(1) Å;
β = 95.04(2)°
Identification
Color Olive-green, yellow-green; green to yellow-green in transmitted light
Crystal habit Aggregates of scaly crystals, rosettes
Crystal system Monoclinic
Cleavage Perfect
Mohs scale hardness
Luster Vitreous, waxy, greasy, pearly
Diaphaneity Translucent
Specific gravity 3.5 - 3.8
Optical properties Biaxial (+/-)
Refractive index nα = 1.793 nβ = 1.801 nγ = 1.816
Birefringence δ = 0.023
Pleochroism Weak
2V angle Measured: 63° to 83°
Solubility Soluble in acids
References [1][2][3]

Volborthite is a mineral containing copper and vanadium, with the formula Cu3V2O7(OH)2·2H2O. Found originally in 1838 in the Urals, it was named for Alexander von Volborth (1800-1876), a Russian paleontologist.

Tangeite (synonym: calciovolborthite), CaCuVO4(OH), is closely related.

Occurrence [edit]

Volborthite was first described in 1837 for an occurrence in the Sofronovskii Mine, Yugovskii Zavod, Perm, Permskaya Oblast, Middle Urals, Russia.[2]

It occurs as an uncommon oxidation mineral in vanadium bearing hydrothermal copper ores. It is associated with brochantite, malachite, atacamite, tangeite, chrysocolla, baryte and gypsum.[1]

References [edit]