
mineral
Likely pyrite-bearing rock
Pyrite (FeS₂), possibly disseminated in a host rock
AI-generated identification · may be incorrectBrassy gray-gold, metallic sparkle, with granular crystals; pyrite has Mohs hardness 6–6.5 and an isometric crystal structure. The image does not show enough detail to identify the host rock or confirm pyrite.
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Physical properties
Brassy gray-gold, metallic sparkle, with granular crystals; pyrite has Mohs hardness 6–6.5 and an isometric crystal structure. The image does not show enough detail to identify the host rock or confirm pyrite.
Formation & geological history
Pyrite forms in hydrothermal veins and sedimentary or metamorphic settings, often through sulfur-bearing fluids reacting with iron. Its age depends on the host deposit.
Uses & applications
Pyrite is collected as a mineral specimen and historically used as a source of sulfur and, less commonly, iron; it is not typically used as jewelry or building stone.
Geological facts
Pyrite is called “fool’s gold,” but is harder and more brittle than gold. Avoid prolonged wet storage, as pyrite can oxidize and deteriorate.
Field identification & locations
The glittering brassy grains suggest pyrite, but a closer view or tests would be needed to distinguish it from other metallic minerals. It occurs worldwide in many rock types.
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