
mineral
White sheet mica (likely muscovite)
Muscovite, KAl₂(AlSi₃O₁₀)(OH)₂
AI-generated identification · may be incorrectPale, translucent-to-white, pearly luster; Mohs hardness 2–2.5. Mica has a layered monoclinic crystal structure and perfect basal cleavage, splitting into thin flexible sheets; the pictured piece appears to be a thin sheet specimen.
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Physical properties
Pale, translucent-to-white, pearly luster; Mohs hardness 2–2.5. Mica has a layered monoclinic crystal structure and perfect basal cleavage, splitting into thin flexible sheets; the pictured piece appears to be a thin sheet specimen.
Formation & geological history
Forms in granites, pegmatites, and metamorphic rocks such as schist, typically during slow cooling or metamorphism. It is common in Precambrian and younger rocks; the specimen’s age cannot be determined from the image.
Uses & applications
Used as an electrical and thermal insulator, filler in paints and cosmetics, and occasionally in crafts or mineral collections.
Geological facts
Muscovite’s name refers to its historic use as window material in Russia. Its exceptionally perfect cleavage lets it peel into remarkably thin sheets.
Field identification & locations
Identify it by its flexible, transparent-to-translucent sheets and easy splitting along flat planes; common sources include India, Brazil, Russia, and the United States. The image alone cannot confirm the mineral, but white sheet mica is the closest match.
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