
metamorphic
Likely pyrite-bearing metamorphic rock
Quartz–mica schist or gneiss with disseminated pyrite (FeS₂)
AI-generated identification · may be incorrectHardness is approximately 6–7 for quartz and 6–6.5 for pyrite; the specimen is gray-brown with brassy metallic grains and a granular, weakly foliated texture. Pyrite is cubic in crystals when well formed, while the surrounding rock commonly contains quartz, mica, and feldspar;…
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Physical properties
Hardness is approximately 6–7 for quartz and 6–6.5 for pyrite; the specimen is gray-brown with brassy metallic grains and a granular, weakly foliated texture. Pyrite is cubic in crystals when well formed, while the surrounding rock commonly contains quartz, mica, and feldspar; specific gravity is roughly 2.7–5.0 depending on pyrite content.
Formation & geological history
Likely formed when clay-rich sediment or igneous rock was buried, heated, and compressed during mountain building; pyrite crystallized in the metamorphic assemblage. Its exact geological age cannot be determined from the photograph.
Uses & applications
Mostly a collector specimen; pyrite may be mined for sulfur and historically for iron, while the host rock can be used as decorative stone but is not typically construction-grade.
Geological facts
The brassy metallic material is likely pyrite, commonly called “fool’s gold,” though the rock may also contain chalcopyrite. Pyrite can tarnish or oxidize in humid conditions, producing acidic minerals.
Field identification & locations
Look for metallic brassy grains, gray quartz-rich matrix, and possible foliation; pyrite leaves a dark greenish-black streak, unlike gold’s yellow streak. Common settings include hydrothermal veins and metamorphic belts worldwide.
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