
mineral
Specular Hematite (Specularite)
Iron Oxide (Fe2O3)
AI-generated identification · may be incorrectHardness: 5.5-6.5 on Mohs scale; Color: Steel-gray to black with a shimmering metallic glitter (specular); Luster: Metallic; Crystal Structure: Trigonal; Cleavage: None (uneven fracture); Specific Gravity: 4.9-5.3.
- Hardness
- 5
- Luster
- Metallic
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Physical properties
Hardness: 5.5-6.5 on Mohs scale; Color: Steel-gray to black with a shimmering metallic glitter (specular); Luster: Metallic; Crystal Structure: Trigonal; Cleavage: None (uneven fracture); Specific Gravity: 4.9-5.3.
Formation & geological history
Formed in high-temperature hydrothermal veins, metamorphic rocks (especially schist), and iron-forming sedimentary sequences. It is often found in banded iron formations (BIFs) dating back over 2 billion years (Precambrian era).
Uses & applications
Primary ore of iron for steel production. In its specular form, it is used for ornamental carvings, jewelry (often called 'Black Diamond'), and as a collector's mineral specimen.
Geological facts
The name comes from the Latin 'speculum,' meaning mirror, because its flat, micaceous crystals are highly reflective. Despite its silver-black appearance, if you rub it against a streak plate, it will leave a characteristic blood-red powder streak.
Field identification & locations
Identify in the field by its distinctive 'glittery' or micaceous appearance and high density (it feels heavy for its size). Look for the cherry-red streak when scratched on unglazed porcelain. Commonly found in Michigan (USA), Brazil, and Magnet Cove, Arkansas.
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