DESCLOIZITE, a rare mineral species consisting of basic lead and zinc vanadate, crystallizing in the orthorhombic system and isomorphous with olivenite. It occurs as small prismatic or pyramidal crystals, usually forming drusy crusts and stalactitic aggregates; also as fibrous encrusting masses with a mammillary surface. The colour 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. A variety known as cuprodescloizite is dull green in colour ; it contains a considerable amount of copper replacing zinc and some arsenic replacing vanadium. Descloizite occurs in veins of lead ores in association with pyromorphite, vanadinite, wulfenite, etc. Localities are the Sierra de Cordoba in Argentina, Lake Valley in Sierra county, New Mexico, Arizona, Phoenix ville in Pennsylvania, Kappel (Eisen-Kappel) near Klagenfurt in Carinthia, and Broken Hill, Rhodesia.