
mineral
Biotite or Phlogopite Mica
K(Mg,Fe)3(AlSi3O10)(F,OH)2
Hardness: 2.5–3.0 on Mohs scale; Color: Dark brown to black (Biotite) or golden-yellow/brown (Phlogopite); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin flexible sheets); Specific Gravity: 2.7–3.3
- Hardness
- 2
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5–3.0 on Mohs scale; Color: Dark brown to black (Biotite) or golden-yellow/brown (Phlogopite); Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin flexible sheets); Specific Gravity: 2.7–3.3
Formation & geological history
Forms in igneous rocks like granite and pegmatites, as well as metamorphic rocks like schist and gneiss. It is common in regional and contact metamorphic zones.
Uses & applications
Used primarily as an insulator in electrical equipment, in joint compound, as a filler in paints and plastics, and as a soil conditioner. High-quality sheets are used in optical instruments.
Geological facts
Commonly confused with gold flakes by novice prospectors due to its golden shimmer in water; however, mica flakes will crumble or shatter when poked with a needle, while gold is malleable.
Field identification & locations
Identify by its 'book-like' appearance and ability to peel into transparent, flexible flakes. Often found in coarse-grained igneous rocks. Check for the pearly luster and perfect cleavage.
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