
mineral
Muscovite Mica
Muscovite (KAl2(AlSi3O10)(OH)2)
Hardness: 2-2.5 on Mohs scale; Color: Colorless, silvery-white, or tan; Luster: Pearly to metallic; Crystal Structure: Monoclinic; Cleavage: Perfect basal cleavage producing thin, flexible sheets; Specific Gravity: 2.8-2.9.
- Hardness
- 2-2
- Color
- Colorless, silvery-white, or tan
- Luster
- Pearly to metallic
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Physical properties
Hardness: 2-2.5 on Mohs scale; Color: Colorless, silvery-white, or tan; Luster: Pearly to metallic; Crystal Structure: Monoclinic; Cleavage: Perfect basal cleavage producing thin, flexible sheets; Specific Gravity: 2.8-2.9.
Formation & geological history
Formed primarily in metamorphic rocks like schists and gneisses, as well as in igneous rocks such as granite and pegmatites. It forms through the metamorphism of clay-rich sediments or the cooling of silica-rich magma fragments.
Uses & applications
Used as an electrical insulator in electronics, as a filler in paints and plastics, and as a glittering agent in makeup (lipstick, eyeshadow) and automotive paints.
Geological facts
Historically called 'Muscovy glass' because it was used in Russia as a cheaper, more durable alternative to glass for windows. Its sheets are highly heat-resistant and do not conduct electricity.
Field identification & locations
Identified in the field by its distinct silvery 'glitter,' pearly luster, and 'peeling' behavior where it flakes off into thin, transparent, elastic plates. Commonly found in micaceous schists and granite outcroppings.
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sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock