
mineral
Muscovite Mica
Muscovite (KAl2(AlSi3O10)(OH)2)
AI-generated identification · may be incorrectHardness: 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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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous