Rock Identifier
Quartz-bearing sulfide ore, possibly pyrite in altered host rock (Likely pyrite (FeS₂) with quartz and possibly calcite or carbonate gangue; exact identification requires testing) — mineral
mineral

Quartz-bearing sulfide ore, possibly pyrite in altered host rock

Likely pyrite (FeS₂) with quartz and possibly calcite or carbonate gangue; exact identification requires testing

AI-generated identification · may be incorrect

Irregular, metallic-to-submetallic specimen with brassy-gold patches, dark sulfide material, and pale gray/beige gangue. Pyrite has Mohs hardness 6–6.5, cubic crystals, poor cleavage, and specific gravity about 5.0; the photograph does not clearly show crystal form.

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Physical properties

Irregular, metallic-to-submetallic specimen with brassy-gold patches, dark sulfide material, and pale gray/beige gangue. Pyrite has Mohs hardness 6–6.5, cubic crystals, poor cleavage, and specific gravity about 5.0; the photograph does not clearly show crystal form.

Formation & geological history

Typically forms in hydrothermal veins, sedimentary replacement deposits, and metamorphic rocks when sulfur-bearing fluids precipitate iron sulfides. Deposits range from ancient Precambrian systems to young active hydrothermal environments.

Uses & applications

Pyrite is mined as a sulfur and occasional gold-associated ore; quartz-bearing pieces are common teaching and collector specimens rather than construction stone.

Geological facts

Often called “fool’s gold,” but pyrite is harder and more brittle than gold and commonly tarnishes to brown or iridescent colors.

Field identification & locations

Look for a brass-yellow metallic color, blackish streak, high density, and brittle fracture; a streak test and hardness test help distinguish it from gold. Common worldwide in hydrothermal and sedimentary ore districts.