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DESCLOIZITE

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Originally appearing in Volume V08, Page 91 of the 1911 Encyclopedia Britannica.
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DESCLOIZITE , a rare See also:

mineral See also:species consisting of basic See also:lead and See also:zinc vanadate, (Pb, Zn)2(OH)VO4, crystallizing in the orthorhombic See also:system and isomorphous with See also:olivenite. It was discovered by A: Damour in 1854, and named by him in See also:honour of the See also:French mineralogist See also: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 See also:surface. The See also:colour is deep See also:cherry-red to See also:brown or See also:black, and the crystals are transparent or translucent with a greasy lustre; the streak is See also:orange-yellow to brown; specific gravity 5.9 to 6.2; hardness 31. A variety known as cuprodescloizite is dull See also:green in colour; it contains a considerable amount of See also:copper replacing zinc and some See also:arsenic replacing See also:Vanadium. Descloizite occurs in See also:veins of lead ores in association with See also:pyromorphite, See also:vanadinite, See also:wulfenite, &c. Localities arethe Sierra de See also:Cordoba in See also:Argentina, See also:Lake Valley in Sierra See also:county, New See also:Mexico, See also:Arizona, See also:Phoenixville in See also:Pennsylvania, and Kappel (Eisen-Kappel) near See also:Klagenfurt in See also:Carinthia. Other names which have been applied to this species are vanadite, tritochorite and ramirite; the uncertain vanadates eusynchite, araeoxene and dechenite are possibly identical with it.

End of Article: DESCLOIZITE

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