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Dominant species
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Descloizite
Descloizite
Chemical
Formula
(Pb,Zn)2VO4OH
Species
Silicates
Crystal
System
Orthorhombic
Mohs
Scale
3
Specific
Gravity
6.1-6.2
Color
Brownish red, red-orange, reddish to blackish brown, nearly black
Streak
Orange to brownish red
Luster
Sub-Vitreous, Resinous, Waxy, Greasy
Refractive
Index
n = 2.185 n = 2.265 n = 2.350
Diaphaneity
Transparent, Translucent
Cleavage
None Observed
Fracture
Irregular/Uneven, Sub-Conchoidal
Crystal Habit:Zoned tabular crystals common, encrustations and plumose aggregates
Geological Setting:Secondary mineral in oxidized zone of vanadium bearing base metal deposits.
Descloizite is a rare mineral species consisting of basic lead and zinc vanadate, (Pb,Zn)2(OH)VO4, crystallizing in the orthorhombic system and isomorphous with olivenite.

The color is deep cherry-red to brown or black, and the crystals are transparent or translucent with a greasy lustre; the streak is orange-yellow to brown; specific gravity 5.9 to 6.2; hardness 31/2. A variety known as cuprodescloizite is dull green in color; it contains a considerable amount of copper replacing zinc and some arsenic replacing vanadium. Appreciable gallium and germanium may also be incorporated into the crystal structure.

Discovery and occurrence

It was discovered in the Sierra de Córdoba deposit in Córdoba, Argentina in 1854 and named in honor of the French mineralogist Alfred Des Cloizeaux. It occurs as small prismatic or pyramidal crystals, usually forming drusy crusts and stalactitic aggregates; also as fibrous encrusting masses with a mammillary surface.

Descloizite occurs in oxidised portions of veins of lead ores in association with pyromorphite, vanadinite, wulfenite, mottramite, mimetite and cerussite.

The Otavi Mountainland of northern Namibia was once considered home to the greatest vanadium deposits in the world, including those at Berg Aukas, Abenab, Baltika and Uitsab. Descloizite and mottramite were the main ore minerals in each of these deposits, which are now exhausted. Other localities are the Sierra de Cordoba in Argentina; Lake Valley in Sierra County, New Mexico; Arizona; Phoenixville in Pennsylvania and Kappel[disambiguation needed] (Eisen-Kappel) near Klagenfurt in Carinthia.