![Muscovite Mica (Muscovite [KAl2(AlSi3O10)(OH)2]) — mineral](https://media.rock.id/muscovite-mica-199a71a4-2656-4542-a71c-c3d79e525550-compressed.jpg)
mineral
Muscovite Mica
Muscovite [KAl2(AlSi3O10)(OH)2]
Hardness: 2-2.5; Color: Colorless, silvery, or light brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal cleavage (peels into thin sheets); Specific gravity: 2.76-3.0
- Hardness
- 2-2
- Color
- Colorless, silvery, or light brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2-2.5; Color: Colorless, silvery, or light brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal cleavage (peels into thin sheets); Specific gravity: 2.76-3.0
Formation & geological history
Formed in igneous environments (pegmatites and granites) and metamorphic rocks (schists and gneisses). It crystallizes from magma or forms through the alteration of other minerals during metamorphism.
Uses & applications
Used as an electrical and thermal insulator in electronics, as a filler in paints and plastics, and in cosmetics (mica powder) for its pearlescent shimmer. Historically used as window panes.
Geological facts
Also known as 'Muscovy glass' because it was used in medieval Russia as a cheap alternative to glass for windows. It is highly heat-resistant and does not conduct electricity.
Field identification & locations
Identify by its 'book' like structure and the ability to peel off elastic, transparent sheets with a fingernail. Commonly found in large flakes within granite pegmatites.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral