- Chromite - Wikipedia
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 Fe Cr 2 O 4
- Chromite: Mineral information, data and localities.
Chromite is the most important chromium ore mineral It forms a complete solid solution series with many other members of the group, eg in the Chromite-Hercynite Series, Chromite-Spinel Series, Chromite-Magnetite Series and the Chromite-Magnesiochromite Series
- Chromite: The only mineral ore of chromium metal - Geology. com
What is Chromite? Chromite is an oxide mineral composed of chromium, iron, and oxygen (FeCr 2 O 4) It is dark gray to black in color with a metallic to submetallic luster and a high specific gravity
- Chromite | Ores, Mining, Processing | Britannica
Chromite, relatively hard, metallic, black oxide mineral of chromium and iron (FeCr2O4) that is the chief commercial source of chromium It is the principal member of the spinel series of chromium oxides; the other naturally occurring member is magnesiochromite, oxide of magnesium and chromium
- Chromite Mineral Data
Named after its chemical composition Comments: Chromite veins in yellow to green antigorite with picrolite, chromian antigorite and dolomite (polished section) Location: Wood's Mine, near 'Texas', Little Britain Township, Lancaster County, Pennsylvania, USA Scale: See Photo
- Chromite - Details and Facts
Chromite is a mineral that is widely used in the metallurgical industry due to its high melting point, resistance to corrosion, and ability to resist wear and tear It is a dark, brownish-black, opaque mineral that is typically found in ultramafic rocks such as serpentinite
- Chromite: The mineral Chromite information and pictures
Detailed description, properties, and locality information guide about the chromium mineral chromite
- Chromite | Chromium Ore, Properties, Uses and Occurrence
Chromite is the most important ore of chromium Crystals are uncommon, but when found they are octahedral Chromite is usually massive or in the form of lenses and tabular bodies, or it may be disseminated as granules It is sometimes found as a crystalline inclusion in diamond
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