
mineral
Hematite
Iron(III) oxide (Fe2O3)
AI-generated identification · may be incorrectHardness: 5.5-6.5 on Mohs scale. Color: Metallic gray to black, often with reddish-brown streaks. Luster: Metallic to submetallic. Crystal structure: Trigonal/Hexagonal. Cleavage: None. Specific gravity: 5.26.
- Hardness
- 5
- Color
- Metallic gray to black, often with reddish-brown streaks
- Luster
- Metallic to submetallic
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Physical properties
Hardness: 5.5-6.5 on Mohs scale. Color: Metallic gray to black, often with reddish-brown streaks. Luster: Metallic to submetallic. Crystal structure: Trigonal/Hexagonal. Cleavage: None. Specific gravity: 5.26.
Formation & geological history
Formed as a primary mineral in igneous rocks or as a secondary mineral in sedimentary iron formations through precipitation from water. Significant deposits formed approximately 2.4 billion years ago during the Great Oxygenation Event.
Uses & applications
Primary ore of iron and steel production. Also used as a pigment in paints (ochre), as polishing rouge, and as a popular semi-precious gemstone for jewelry and beads.
Geological facts
Hematite gets its name from the Greek word for blood (haima) because of its red streak. It is often found in massive quantities on the surface of Mars, giving the planet its characteristic red color.
Field identification & locations
Identify in the field by rubbing the specimen against a porcelain streak plate; it will always leave a reddish-brown streak regardless of the surface color. Commonly found in locations like the Lake Superior district, Brazil, and Australia.
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