Online Encyclopedia

VANADINITE

Online Encyclopedia
Originally appearing in Volume V27, Page 878 of the 1911 Encyclopedia Britannica.
Spread the word: del.icio.us del.icio.us it!

VANADINITE  , a

See also:
mineral consisting of 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 groups also occur . The colour is usually
See also:
light 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 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 Klagenfurt in Carinthia, Arizona and New Mexico . (L . J .

End of Article: VANADINITE
[back]
VAN WERT
[next]
VANADIUM

Additional information and Comments

There are no comments yet for this article.
» Add information or comments to this article.
Please link directly to this article:
Highlight the code below, right click and select "copy." Paste it into a website, email, or other HTML document.