CHROMITE
, a member of the See also:spinel See also:group of minerals; an See also:oxide of See also:chromium and ferrous See also:iron, FeCr2O4
.
It is also known as chromic iron or as chrome-iron-ore, and is the See also:chief commercial source of chromium and its compounds
.
It crystallizes in See also:regular octahedra, but is usually found as grains or as granular to compact masses
.
In its iron-See also:black See also:colour with submetallic lustre and See also:absence of cleavage it resembles See also:magnetite (magnetic iron-ore) in See also:appearance, but differs from this in being only slightly if at all magnetic and in the See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
brown colour of its See also:powder
.
The hardness is 51; specific gravity 4.5
.
The theoretical See also:formula FeCr2O4 corresponds with chromic oxide (Cr203) 68%, and ferrous oxide 32%; the ferrous oxide is, however, usually partly replaced by See also:magnesia, and the chromic oxide by alumina and ferric oxide, so that there may be a See also:gradual passage to picotite or chromespinel
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Much of the material See also:mined as ore does not contain more than 40 to 50% of chromic oxide
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In the See also:form of isolated grains the See also:mineral is a characteristic constituent of ultrabasic igneous rocks, namely the peridotites and the serpentines which have resulted from their alteration
.
It is also found under similar conditions in meteoric stones and irons
.
Often these rocks enclose large segregated masses of granular chromite
.
The earliest worked deposits were those in the See also:serpentine of the See also:Bare Hills near See also:Baltimore, See also:Maryland, U.S.A.; it was also formerly extensively mined in See also:Lancaster See also:county, See also:Pennsylvania, and is now mined in See also:California, as well as in See also:Turkey, the Urals, Dun See also:Mountain near See also:Nelson in New See also:Zealand, and Unst in the Shetlands
.
Chrome-iron-ore is largely used in the preparation of chromium compounds for use as See also:pigments (chrome-yellow, &c.) and in See also:calico-See also:printing; it is also used in the manufacture of chrome-See also:steel
.
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