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1 See Also  





2 References  





3 External links  














Crocoite






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From Wikipedia, the free encyclopedia
 


This is an old revision of this page, as edited by Ponyo (talk | contribs)at18:27, 12 May 2007 (Removed outdated stub tag). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
(diff)  Previous revision | Latest revision (diff) | Newer revision  (diff)

Crocoite specimen from the Red Lead Mine, Tasmania, Australia
Crocoite from Dundas, Tasmania.
Crystal intergrowth of the secondary lead mineral crocoite

Crocoite is a mineral consisting of lead chromate, PbCrO4, and crystallizing in the monoclinic system. It is sometimes used as a paint, being identical in composition with the artificial product chrome yellow; it is the only chromate of any importance found in nature. It was discovered at Berezovsk near Ekaterinburg in the Urals in 1766; and named crocoise by F. S. Beudant in 1832, from the Greek if peoc, saffron, in allusion to its color, a name first altered to crocoisite and afterwards to crocoite. It is found as well-developed crystals, but there are most often poorly terminated, and are of a bright hyacinth-red color, which are translucent and have an adamantine to vitreous lustre. On exposure to light much of the translucency and brilliancy is lost. The streak is orange-yellow; Mohs hardness is 2.5-3; and the specific gravity is 6.0. In the Urals the crystals are found in quartz-veins traversing graniteorgneiss. Other localities which have yielded good crystallized specimens are Congonhas do Campo near Ouro Preto in Brazil, Luzon in the Philippines, and Umtali in Mashonaland.

Gold is often found associated with this mineral. Crystals far surpassing in beauty any previously known have been found in the Adelaide Mine at Dundas, Tasmania; they are long slender prisms, 3 or 4 in. in length, with a brilliant lustre and color. Crocoite is also the official Tasmanian mineral emblem.

Associated with crocoite at Berezovsk are the closely allied minerals phoenicochroite and vauquelinite. The former is a basic lead chromate, Pb2CrO5, and the latter a lead and copper phosphate-chromate, Pb2CuCrO4PO4OH. Vauquelinite forms brown or green monoclinic crystals, and was named after L. N. Vauquelin, who in 1797 discovered (simultaneously with and independently of M. H. Klaproth) the element chromium in crocoite.

See Also

References

External links


Retrieved from "https://en.wikipedia.org/w/index.php?title=Crocoite&oldid=130370420"

Categories: 
Lead minerals
Chromium minerals
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CS1 errors: missing title
Wikipedia articles incorporating a citation from the 1911 Encyclopaedia Britannica with no article parameter
Wikipedia articles incorporating text from the 1911 Encyclopædia Britannica
 



This page was last edited on 12 May 2007, at 18:27 (UTC).

This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



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