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VANADINITE , a See also: mineral consisting of See also: lead chloro-vanadate, (PbCl)Pb4(VO4)3, crystallizing in the hexagonal See also: system and isomorphous with See also: pyromorphite and See also: mimetite (q.v.)
.
The crystals are usually six-sided prisms terminated by the basal planes, but are sometimes modified by numerous pyramidal planes which exhibit parallel hemihedrism
.
Rounded crystals and See also: groups also occur
.
The colour is usually See also: light See also: brown or yellow, but crystals from Arizona are bright red
.
Owing to isomorphous replacement of the
See also: vanadium by phosphorus and arsenic, the specific gravity varies from 6.6 to 7•2; a variety containing much arsenic is called endlichite
.
The hardness is 3
.
The mineral is one of secondary formation in See also: veins of lead ore
.
It was first found in Mexico, and in 1801 was asserted to contain a new See also: element, which was called " erythronium "; this was later proved to be identical with the subsequently discovered element vanadium
.
Other well-known localities are Wanlockhead in See also: Dumfriesshire, Kappel (Eisen-Kappel), near See also: Klagenfurt in See also: Carinthia, Arizona and New Mexico
.
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