
mineral
Muscovite Mica
Muscovite / KAl2(AlSi3O10)(OH)2
AI-generated identification · may be incorrectHardness: 2.5 on Mohs scale; Color: Colorless, silver-gray, or pale green; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin flexible sheets); Specific gravity: 2.82
- Hardness
- 2
- Color
- Colorless, silver-gray, or pale green
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5 on Mohs scale; Color: Colorless, silver-gray, or pale green; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin flexible sheets); Specific gravity: 2.82
Formation & geological history
Formed in igneous and metamorphic environments. Mostly found in pegmatites, granites, and regional metamorphic rocks like schist and phyllite. Geological age varies across eras depending on host rock formation.
Uses & applications
Used as an electrical insulator in electronics, a pearlescent pigment in makeup, a heat-resistant material for stove windows, and an additive in joint compound and paints.
Geological facts
Historically called 'Muscovy glass' because it was used as window panes in medieval Russia. It is highly elastic, meaning the sheets can be bent and will spring back to their original shape.
Field identification & locations
Identify in the field by its distinct 'books' of thin, transparent, flaky sheets that can be peeled with a fingernail. Commonly found in Brazil, India, and the United States (specifically North Carolina and South Dakota).
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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