
mineral
Iron sulfide-rich ore, possibly pyrite-bearing gossan
Likely pyrite (FeS₂) with iron oxides/hydroxides and host rock; exact identification requires testing
AI-generated identification · may be incorrectBrassy yellow metallic patches contrast with dark gray-purple, earthy material; likely Mohs 6–6.5 for pyrite, with metallic luster and cubic crystal structure, though much is massive or weathered. Specific gravity may be roughly 4.8–5.0 where pyrite is abundant.
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Physical properties
Brassy yellow metallic patches contrast with dark gray-purple, earthy material; likely Mohs 6–6.5 for pyrite, with metallic luster and cubic crystal structure, though much is massive or weathered. Specific gravity may be roughly 4.8–5.0 where pyrite is abundant.
Formation & geological history
Probably formed by hydrothermal mineralization or sulfide-vein oxidation; geological age cannot be determined from the photograph. Weathering of sulfides commonly produces yellow-brown iron oxyhydroxides and porous gossan.
Uses & applications
Used historically as a sulfur and iron source and commonly collected as an ore specimen; unattractive or weathered material generally has little jewelry or construction value.
Geological facts
Pyrite is often called “fool’s gold,” but its brassy color and high hardness distinguish it from native gold. Acid drainage can develop when sulfide-rich ore weathers.
Field identification & locations
Identify with a streak test, hardness test, density, and ideally X-ray diffraction: pyrite gives a dark greenish-black streak and does not scratch easily with steel. Common in hydrothermal veins, sedimentary beds, and metamorphic sulfide deposits worldwide.
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