
mineral
Pyrite (fool’s gold)
Pyrite, iron disulfide (FeS₂)
AI-generated identification · may be incorrectBrassy-gold metallic luster with blocky, reflective crystal faces. Mohs hardness 6–6.5; cubic crystal system, typically no prominent cleavage; specific gravity about 5.0.
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Physical properties
Brassy-gold metallic luster with blocky, reflective crystal faces. Mohs hardness 6–6.5; cubic crystal system, typically no prominent cleavage; specific gravity about 5.0.
Formation & geological history
Forms when iron and sulfur combine in low-oxygen settings, including hydrothermal veins and sedimentary rocks. Pyrite occurs across a wide range of geological ages.
Uses & applications
Used as a source of sulfur for sulfuric acid and collected as a common mineral specimen; historically used to produce sparks.
Geological facts
Its metallic appearance can resemble gold, but pyrite is harder and more brittle. The specimen appears to be a small cluster of intergrown crystals.
Field identification & locations
Look for brassy color, cubic faces, and brittle fracture; unlike gold, pyrite can leave a dark greenish-black streak. Common worldwide in veins, coal beds, and sedimentary formations.
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