
metamorphic
Likely muscovite-bearing mica schist
Mica schist, composed chiefly of muscovite (KAl₂(AlSi₃O₁₀)(OH)₂) and quartz; exact identification is uncertain from the image alone.
AI-generated identification · may be incorrectPale silvery-gray with a pearly sheen and flaky, foliated texture. Muscovite has Mohs hardness 2–2.5 and perfect basal cleavage; quartz is harder (7).
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Physical properties
Pale silvery-gray with a pearly sheen and flaky, foliated texture. Muscovite has Mohs hardness 2–2.5 and perfect basal cleavage; quartz is harder (7).
Formation & geological history
Forms when clay-rich sedimentary rocks undergo regional metamorphism, aligning mica flakes into layers. Its age cannot be determined from appearance; schists occur in many ancient mountain belts.
Uses & applications
Mica is used in electrical and heat-resistant products; schist is mainly a decorative or landscaping stone, and attractive specimens are collected.
Geological facts
The reflective plates are consistent with mica, which splits into extremely thin, flexible sheets.
Field identification & locations
Look for platy flakes that glint and separate along foliation; a scratch or cleavage test can help distinguish mica-rich schist from other silvery rocks. Mica schists occur worldwide in metamorphic terrains.
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