
mineral
Muscovite Mica
Muscovite (KAl2(AlSi3O10)(OH)2)
Hardness: 2-2.5 on Mohs scale; Color: Colorless, silvery-white, or light brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic (tabular/foliated); Cleavage: Perfect basal (can be peeled into thin sheets); Specific gravity: 2.76-3.0
- Hardness
- 2-2
- Color
- Colorless, silvery-white, or light brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2-2.5 on Mohs scale; Color: Colorless, silvery-white, or light brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic (tabular/foliated); Cleavage: Perfect basal (can be peeled into thin sheets); Specific gravity: 2.76-3.0
Formation & geological history
Formed in igneous or metamorphic environments. It is a common constituent of granitic pegmatites, schists, and gneisses, often resulting from the metamorphism of argillaceous rocks.
Uses & applications
Used primarily as an electrical insulator in capacitors and high-voltage equipment, a lubricant, a filler in paints and plastics, and in cosmetics for pearlescent shimmer.
Geological facts
In early Russia, it was known as 'Muscovy glass' because it was used as a window material. It is heat resistant and transparent in thin sheets, making it ideal for ancient wood-stove windows.
Field identification & locations
Identify by its perfect cleavage that allows you to peel off thin, flexible, elastic sheets with a fingernail. Commonly found in mountainous regions globally, particularly in pegmatite veins.
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Schist
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Epidote
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Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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Biotite Schist
Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]
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