
mineral
Muscovite Mica
Muscovite - KAl2(AlSi3O10)(F,OH)2
AI-generated identification · may be incorrectHardness: 2-2.5 on Mohs scale. Color: Pale green to silvery white/tan, transparent to translucent. Luster: Pearly to vitreous. Crystal system: Monoclinic. Cleavage: Perfect basal cleavage forming flexible, elastic sheets.
- Hardness
- 2-2
- Color
- Pale green to silvery white/tan, transparent to translucent
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2-2.5 on Mohs scale. Color: Pale green to silvery white/tan, transparent to translucent. Luster: Pearly to vitreous. Crystal system: Monoclinic. Cleavage: Perfect basal cleavage forming flexible, elastic sheets.
Formation & geological history
Forms primarily in regional metamorphic rocks like schists and gneisses, as well as in igneous pegmatites and granites under moderate to high temperatures and pressure.
Uses & applications
Widely used as an electrical and thermal insulator, in makeup/cosmetics for shimmer, as a joint compound filler, and in paint manufacturing.
Geological facts
Muscovite was historically used as a glass substitute for windows in medieval Russia, which inspired its name (derived from Muscovy glass). Sheets can be peeled into paper-thin, see-through layers.
Field identification & locations
Identified by its distinctive micaceous structure, allowing it to split into extremely thin, flexible, transparent sheets. Commonly found in pegmatite deposits worldwide (e.g., Brazil, India, USA, Madagascar).
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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