| Name: Hematite |
Origin of name: from Greek haima(t), meaning blood, because of the colour of the powdered mineral |
Chemical composition: Fe2O3 |
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Hematite, an oxide of iron, is a very common mineral and the main ore of iron. It occurs in hydrothermal veins and in sedimentary deposits, and is also found as a minor constituent of some igneous rocks.
Crystals of hematite are usually tabular or rhombohedral, but massive, granular, fibrous and reniform habits are more common; reniform hematite, as shown here, is also known as "kidney-ore". Hematite has been mined since ancient times; iron production was widespread by 500 BC. The powdered mineral has long been used as a red pigment in paint and cosmetics; it is also used as a fine abrasive (jewellers' rouge). |
Crystal system: trigonal/hexagonal |
| Class: Oxides |
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| Hardness: 5.0-6.0 |
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| Cleavage: none |
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| Colour: grey, black or blood-red |
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| Specific gravity: 5.26 |