Muscovite

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Muscovite

Muscovite from a pegmatite outcrop along the Patapsco River in Baltimore County, Maryland.
General
Category Mineral Species
Chemical formula KAl2(AlSi3O10)(F,OH)2
Identification
Molecular Weight 398.71 gm
Color White, grey, silvery
Crystal habit massive to platy Crystaline
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, 4
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
Density 2.83 g/cm3
Melting point approximately 1320°C
Diaphaneity transparent or translucent
References [1][2]

Muscovite (also known as Common mica, Isinglass, or Potash mica[3]) is a phyllosilicate mineral of aluminium and potassium with formula: KAl2(AlSi3O10)(F,OH)2. It has a highly perfect basal cleavage yielding remarkably thin laminae (sheets), which are often highly elastic. Sheets of muscovite 5 metres by 3 metres have been found in Nellore, India.[4]

Muscovite melts at approximately 1320°C, 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 quite a high birefringence. Its crystal system is monoclinic.

[edit] See also

[edit] References

  1. ^ Muscovite: Muscovite mineral information and data
  2. ^ Muscovite Mineral Data
  3. ^ Encyclopædia Britannica
  4. ^ The Complete Encyclopedia of Minerals by P. Korbel and M. Novak
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