
metamorphic
Likely pyrite-bearing metamorphic rock
Quartz–mica schist or phyllite with disseminated pyrite (FeS₂)
AI-generated identification · may be incorrectDark gray-green, foliated, and sparkly with brassy metallic patches; likely hardness 2–6 depending on minerals, with uneven fracture and moderate-to-high density. The brassy grains may be pyrite, but image resolution prevents confident mineral identification.
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Physical properties
Dark gray-green, foliated, and sparkly with brassy metallic patches; likely hardness 2–6 depending on minerals, with uneven fracture and moderate-to-high density. The brassy grains may be pyrite, but image resolution prevents confident mineral identification.
Formation & geological history
Probably formed when clay-rich sediment was buried, heated, and compressed during regional metamorphism; its exact geological age and locality cannot be determined from the photograph.
Uses & applications
Primarily a teaching or collecting specimen; pyrite-bearing schist may be used locally as decorative stone, but it is generally unsuitable for high-value jewelry or construction.
Geological facts
Pyrite is iron sulfide, FeS₂, commonly called “fool’s gold.” Unlike gold, it is brittle, commonly forms cubic crystals, and can produce a dark streak rather than a yellow metallic streak.
Field identification & locations
Look for planar foliation, sparkly mica, and brassy grains; a streak test, hardness test, magnet test, and acid reaction would help distinguish pyrite-bearing schist from sulfide-rich ore or slag. Similar rocks occur in metamorphic belts worldwide.
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