
mineral
Mica
Phyllosilicate (group name), typically Muscovite KAl2(AlSi3O10)(OH)2 or Biotite K(Mg,Fe)3(AlSi3O10)(OH)2
Hardness: 2.0–4.0; Color: Silvery-gray, brownish, or black; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.7–3.1
- Hardness
- 2
- Color
- Silvery-gray, brownish, or black
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.0–4.0; Color: Silvery-gray, brownish, or black; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific gravity: 2.7–3.1
Formation & geological history
Formed in igneous environments (granites, pegmatites) and metamorphic rocks (schists, gneisses) through cooling of magma or under high pressure and temperature conditions.
Uses & applications
Used as an electrical insulator in electronics, as a filler in paints and plastics, in joint compounds for drywall, and in cosmetics for its pearlescent shimmer.
Geological facts
Mica is famous for its 'books' or stacks of sheets that can be peeled away. During World War II, mica was considered a strategic material due to its heat resistance and electrical insulation properties.
Field identification & locations
Identify in the field by its distinct flaky texture and shiny, metallic luster. It can be easily scratched with a fingernail and splits into flexible, elastic layers. Commonly found in sparkling river sands or embedded in crystalline rocks.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Biotite Schist
Biotite-rich Schist [K(Mg,Fe)3AlSi3O10(F,OH)2]
metamorphic
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral