
metamorphic
Mica-rich schist (likely biotite schist)
Mica schist, composed mainly of biotite and/or muscovite with quartz and feldspar
AI-generated identification · may be incorrectGlittery, strongly foliated texture with brown-gold mica flakes and darker grains. Mica is Mohs 2–3 with perfect basal cleavage; quartz, if present, is Mohs 7. Exact minerals cannot be confirmed from the photo.
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Physical properties
Glittery, strongly foliated texture with brown-gold mica flakes and darker grains. Mica is Mohs 2–3 with perfect basal cleavage; quartz, if present, is Mohs 7. Exact minerals cannot be confirmed from the photo.
Formation & geological history
Formed when mica-rich sedimentary or igneous rock underwent heat and pressure, causing minerals to recrystallize and align. Its age and specific formation setting cannot be determined visually.
Uses & applications
Schist is used locally as decorative stone and aggregate; attractive mica-rich pieces are mainly collected as geological specimens.
Geological facts
The visible sparkle likely comes from reflective mica flakes, while the dark grains may be biotite or another accessory mineral.
Field identification & locations
Look for glittering platy minerals and a layered or foliated fabric; schist is common in metamorphic mountain belts worldwide. A hand specimen or mineral tests would be needed for a confident identification.
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