
mineral
Hematite
Iron(III) oxide (Fe2O3)
AI-generated identification · may be incorrectHardness: 5.5-6.5 on Mohs scale; Color: Steel-gray to black in crystals, dull red in earthy forms; Luster: Metallic to sub-metallic; Crystal structure: Trigonal; Cleavage: None; Specific gravity: 5.26
- Hardness
- 5
- Color
- Steel-gray to black in crystals, dull red in earthy forms
- Luster
- Metallic to sub-metallic
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Physical properties
Hardness: 5.5-6.5 on Mohs scale; Color: Steel-gray to black in crystals, dull red in earthy forms; Luster: Metallic to sub-metallic; Crystal structure: Trigonal; Cleavage: None; Specific gravity: 5.26
Formation & geological history
Formed in sedimentary environments via precipitation in water, as well as in igneous and metamorphic rocks through hydrothermal processes. Significant deposits date back to the Banded Iron Formations of the Proterozoic eon.
Uses & applications
Primary ore of iron; used in heavy industry for steel production. It is also used in jewelry (beads and cabochons), as an abrasive (jeweler's rouge), and as a pigment in paints and cosmetics.
Geological facts
Hematite is known for its 'blood-red' streak when scratched on a porcelain plate, even if the specimen looks metallic black. It is also the mineral responsible for the reddish tint of the Martian surface.
Field identification & locations
Identify in the field by its high density (feels heavy for its size) and its distinct reddish-brown streak. Common locations include the Lake Superior region (USA), Brazil, Australia, and China.
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