
mineral
Hematite
Iron(III) oxide (Fe2O3)
AI-generated identification · may be incorrectHardness: 5.5 to 6.5 on the Mohs scale. Color: Dark steel-gray, silver, reddish-brown, or black. Luster: Metallic to submetallic or earthy. Crystal System: Trigonal. Cleavage: None, exhibits uneven to conchoidal fracture. Specific Gravity: 5.26.
- Hardness
- 5
- Color
- Dark steel-gray, silver, reddish-brown, or black
- Luster
- Metallic to submetallic or earthy
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Physical properties
Hardness: 5.5 to 6.5 on the Mohs scale. Color: Dark steel-gray, silver, reddish-brown, or black. Luster: Metallic to submetallic or earthy. Crystal System: Trigonal. Cleavage: None, exhibits uneven to conchoidal fracture. Specific Gravity: 5.26.
Formation & geological history
Formed in a variety of environments, notably hydrothermal veins, sedimentary beds, and as an alteration product of other iron-bearing minerals. Can range in geological age from Precambrian banded iron formations billions of years old to modern deposits.
Uses & applications
Primary ore of iron; used in heavy media separation, radiation shielding, pigment production, and occasionally polished for jewelry and ornamental carvings.
Geological facts
Hematite leaves a distinctive reddish-brown streak when scratched across unglazed porcelain, a key diagnostic test that sets it apart from other dark metallic minerals like magnetite.
Field identification & locations
Identify by its heavy weight for its size, reddish-brown streak, and lack of strong magnetism. Found worldwide, with major deposits in Australia, Brazil, China, and the United States (Lake Superior region).
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