Chromite

Chromite is a crystalline mineral composed primarily of iron(II) oxide and chromium(III) oxide compounds. It can be represented by the chemical formula of FeCr2O4. It is an oxide mineral belonging to the spinel group. The element magnesium can substitute for iron in variable amounts as it forms a solid solution with magnesiochromite (MgCr2O4). A substitution of the element aluminium can also occur, leading to hercynite (FeAl2O4). Chromite today is mined particularly to make stainless steel through the production of ferrochrome (FeCr), which is an iron-chromium alloy.

Chromite
Octahedral chromite crystal from the Freetown Layered Complex in Sierra Leone, Africa (size: 1.3 x 1.2 x 1.2 cm)
General
CategoryOxide minerals
Spinel group
Spinel structural group
Formula
(repeating unit)
(Fe, Mg)Cr2O4
IMA symbolChr
Strunz classification4.BB.05
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H-M symbol: (4/m 3 2/m)
Space groupFd3m (no. 227)
Unit cella = 8.344 Å; Z = 8
Identification
ColorBlack to brownish black; brown to brownish black on thin edges in transmitted light
Crystal habitOctahedral rare; massive to granular
TwinningSpinel law on {Ill}
CleavageNone, parting may develop along {III}
FractureUneven
TenacityBrittle
Mohs scale hardness5.5
LusterResinous, Greasy, Metallic, Sub-Metallic, Dull
StreakBrown
DiaphaneityTranslucent to opaque
Specific gravity4.5–4.8
Optical propertiesIsotropic
Refractive indexn = 2.08–2.16
Other characteristicsWeakly magnetic
References

Chromite grains are commonly found in large mafic igneous intrusions such as the Bushveld in South Africa and India. Chromite is iron-black in color with a metallic luster, a dark brown streak and a hardness on the Mohs scale of 5.5.

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