Chemical Formula |
Fe2O3 |
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Composition |
Iron oxide. May contain slight amounts of titanium. |
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Variable Formula |
(Fe,Ti)2O3 |
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Color |
Black, gray to silver gray, brown to reddish brown, red. Some specimens are iridescent, and other are multicolored or banded gray and dark red. |
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Streak |
Red to reddish brown |
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Hardness |
5 - 6 |
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Crystal System |
Hexagonal |
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Crystal Forms |
Crystals occurs in thin plates, as well as bundles of small micaceous plates, and in thin splinters. Most commonly massive, mammilary, botryoidal, reniform, oolitic, stalactitic, and radiating. Scalenohedraland rhombohedral crystals occur, as well as tabular and groups of tabular crystals. Crystals are oftenstriated. Dendritic and rosette forms are also found. May form as a pseudomorph after other minerals, especially as octahedral crystals of Magnetite. |
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Transparency |
Opaque |
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Specific Gravity |
4.9 - 5.3 |
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Luster |
Metallic to dull |
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Cleavage |
None, but occasionally exhibits rhombohedral and basal parting. |
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Fracture |
Uneven |
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Tenacity |
Brittle |
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Other ID Marks |
Hematite is paramagnetic, meaning it is slightly attracted to magnetic fields. |
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Complex Tests |
Becomes strongly magnetic when heated. |
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In Group |
Oxides; Simple Oxides |
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Striking Features |
Reddish streak, hardness, crystal habits, and paramagnetism |
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Environment |
Occurs in almost all different environments. |
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Rock Type |
Igneous, Sedimentary, Metamorphic |
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Popularity (1-4) |
1 |
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Prevalence (1-3) |
1 |
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Demand (1-3) |
1 |
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