
metamorphic
Pyrite-bearing schist (likely gold- or sulfide-bearing ore)
Pyrite, FeS₂, in micaceous schist; exact identification requires testing
AI-generated identification · may be incorrectGray-brown, foliated matrix with brassy metallic flakes and glittering surfaces, consistent with pyrite in mica-rich schist. Pyrite hardness is 6–6.5 Mohs, metallic luster, cubic crystal structure, and specific gravity about 5.0; the host schist is softer and splits along foliation.
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Physical properties
Gray-brown, foliated matrix with brassy metallic flakes and glittering surfaces, consistent with pyrite in mica-rich schist. Pyrite hardness is 6–6.5 Mohs, metallic luster, cubic crystal structure, and specific gravity about 5.0; the host schist is softer and splits along foliation.
Formation & geological history
Formed when sulfide-bearing sediments or volcanic material were metamorphosed, concentrating pyrite along foliation; age depends on locality and cannot be determined from the image. The yellow metallic grains may also include chalcopyrite or native gold, which cannot be confirmed visually.
Uses & applications
Collected as an ore specimen; pyrite is mined for sulfur and historically for sulfuric-acid production, while schist has limited decorative or aggregate use. Any gold value depends on assay rather than appearance.
Geological facts
Pyrite’s brassy color commonly causes confusion with gold, but pyrite is brittle and leaves a dark streak, whereas gold is malleable and leaves a yellow streak.
Field identification & locations
Check for foliation, metallic brassy grains, brittleness, and streak on unglazed porcelain; use hardness, density, acid, and laboratory assay to distinguish pyrite, chalcopyrite, and gold. Common in metamorphic belts and hydrothermal ore deposits worldwide.
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