
mineral
Muscovite Mica
Muscovite (Potassium Aluminum Silicate) - KAl2(AlSi3O10)(F,OH)2
AI-generated identification · may be incorrectHardness: 2.0–2.5 Mohs (scratches with fingernail). Color: Colorless, silvery, or light green. Luster: Pearly to Vitreous. Crystal Structure: Monoclinic, typically forming thin, flexible, elastic sheets or flakes. Cleavage: Perfect basal cleavage.
- Hardness
- 2
- Color
- Colorless, silvery, or light green
- Luster
- Pearly to Vitreous
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Physical properties
Hardness: 2.0–2.5 Mohs (scratches with fingernail). Color: Colorless, silvery, or light green. Luster: Pearly to Vitreous. Crystal Structure: Monoclinic, typically forming thin, flexible, elastic sheets or flakes. Cleavage: Perfect basal cleavage.
Formation & geological history
Formed as a primary mineral in igneous rocks like granite and pegmatites, as well as in metamorphic rocks like schist and phyllite during regional metamorphism.
Uses & applications
Used as an electrical insulator in electronics, as a heat-resistant window material (Isinglass), in makeup for shimmer, and as a filler in paints and plastics.
Geological facts
Muscovite was once used for windows in Russia because it was cheaper and more heat-resistant than glass; the name 'Muscovite' comes from 'Muscovy-glass'. Single sheets can be peeled off almost infinitely thin.
Field identification & locations
Identify by its ability to peel into flexible, transparent thin sheets and its pearly luster. Commonly found in coarse-grained granites and shiny schists worldwide.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary