
mineral
Muscovite Mica
Muscovite (KAl2(AlSi3O10)(OH)2)
AI-generated identification · may be incorrectHardness: 2-2.5; Color: Colorless, silvery-white, or light gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.76–3.0
- Hardness
- 2-2
- Color
- Colorless, silvery-white, or light gray
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2-2.5; Color: Colorless, silvery-white, or light gray; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.76–3.0
Formation & geological history
Commonly formed in igneous rocks like granites and pegmatites, and in metamorphic rocks like schists and gneisses through regional metamorphism. It forms under a wide range of temperatures and pressures.
Uses & applications
Used as an electrical and thermal insulator in electronics, as a filler in paints and plastics, in joint compounds for drywall, and as 'glitter' in cosmetics like eyeshadow and nail polish.
Geological facts
In medieval Russia, large sheets of muscovite were used for windows as a cheaper alternative to glass, which is why it was historically called 'Muscovy-glass'. Due to its heat resistance, it was also used for wood-stove windows.
Field identification & locations
Identify in the field by its distinct ability to peel into thin, flexible, transparent sheets and its pearly, reflective luster. It is ubiquitous in crushed granite gravel and mountain outcrops.
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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