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Muscovite
Muscovite from a pegmatite outcrop along the Patapsco River in Baltimore County, Maryland.
General
Category Silicate mineral
Chemical formula KAl2(AlSi3O10)(F,OH)2
Identification
Color White, grey, silvery
Crystal habit massive to platy
Crystal system Monoclinic - prismatic
Twinning common on the [310] less common on the {001}
Cleavage Perfect on the {001}
Fracture Micaeous
Tenacity Elastic
Mohs Scale hardness 2–2.5 parallel to {001} to 4 right angle to {001}
Luster Vitreous
Refractive index nα = 1.552–1.576 nβ = 1.582–1.615 nγ = 1.587–1.618
Optical Properties Biaxial (-)
Birefringence δ = 0.035 - 0.042
Dispersion r > v weak
Pleochroism weak when colored
Ultraviolet fluorescence None
Streak White
Specific gravity 2.76–3
Diaphaneity transparent to translucent
References 123

Muscovite (also known as Common mica, Isinglass, or Potash mica4) is a phyllosilicate mineral of aluminium and potassium with formula KAl2(AlSi3O10)(F,OH)2, or (KF)2(Al2O3)3(SiO2)6(H2O). It has a highly-perfect basal cleavage yielding remarkably-thin laminæ (sheets) which are often highly elastic. Sheets of muscovite 5 metres by 3 metres have been found in Nellore, India.5

Muscovite has a Mohs hardness of 2–2.25 parallel to the [001] face, 4 perpendicular to the [001] and a specific gravity of 2.76–3. It can be colorless or tinted through grays, browns, greens, yellows, or (rarely) violet or red, and can be transparent or translucent. The green, chromium-rich variety is called fuchsite.

Muscovite is the most common mica, found in granites, pegmatites, gneisses, and schists, and as a contact metamorphic rock or as a secondary mineral resulting from the alteration of topaz, feldspar, kyanite, etc. In pegmatites, it is often found in immense sheets that are commercially valuable. Muscovite is in demand for the manufacture of fireproofing and insulating materials and to some extent as a lubricant.

The name of muscovite comes from Muscovy-glass, a name formerly used for the mineral because of its use in Russia for windows. It is anisotropic and has high birefringence. Its crystal system is monoclinic.

See also

References

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