Muscovite

KAl2(Si3Al)O10(OH)2
IMA status
  • Approved
  • Grandfathered
IMA symbol
Ms
Also known as
  • Ammochrysos
  • Amphilogite
  • Antonit
  • +12 more

History

The name muscovite is a memory of a Russian trade. Before glass became cheap, sheets of this mineral did the work of windows — clear, tough, splittable into panes by the thumb.

Mica in the general sense was known to ancient Indian, Egyptian, Greek, Roman, and Chinese civilisations, and to the Aztecs. Several pre-modern names for what would become muscovite circulated through European texts in the seventeenth century and before: Muscovy Glass, Cat Silver, and lapis specularisstone mirror.

The English name came from a Tudor diplomat's mailbag. Sheets of the mineral were imported from the Russian province of Muscovy, where they served as a cheaper substitute for window glass. The English term Muscovy-glass first appears in letters from 1568 written by George Turberville, secretary to England's ambassador at the court of Tsar Ivan the Terrible.

By the early eighteenth century, English mineralogy had begun catching the mineral under three further names. Mica and glimmer both surface in Phillips and Kersey's 1706 dictionary; isinglass follows in 1747, on the record of the Oxford English Dictionary. Isinglass arrived by an odd transfer — the word had previously meant a gelatinous bladder taken from sturgeon, and only later was applied to thin transparent mineral sheets that looked similar.

The standalone name muscovite entered scientific use in 1794, when the mineralogist Johann Gottfried Schmeisser used it in his System of Mineralogy. The form was derived directly from Muscovy glass, the older trade name that was still in common use at the time.

Industrial & practical applications

Muscovite reaches industry in two very different forms. Large transparent sheets, split by hand from a single crystal, supply the electrical and high-temperature trades. Ground powder, milled from smaller fragments, goes into paints, plastics, drywall, and cosmetics.

Sheet mica

Muscovite is the principal mica used by the electrical industry. Its thin sheets work as a dielectric — the insulating layer that separates charged plates — in capacitors built for high-frequency and radio-frequency use. Only the highest-quality grade, known in the trade as India ruby mica or ruby muscovite mica, is selected for this role.

Cleavability and heat tolerance suit the same sheets to other duties. They line the gauge glasses of high-pressure steam boilers, where flexibility, transparency, and resistance to heat together matter. They substitute for glass in industrial furnace and oven windows, and in the small peepholes of stoves and lanterns where ordinary glass would crack.

Ground mica

Ground muscovite is consumed in much larger volume than sheet, but for less glamorous ends. The single biggest outlet, in the United States, is the joint compound used to fill and finish seams in gypsum wallboard — drywall. In 2008, joint compound accounted for 54 percent of all dry-ground mica consumption.

Paint is the second outlet. Ground mica serves as a pigment extender — a low-cost filler that bulks out the pigment without dulling its colour — and took 22 percent of dry-ground supply in 2008. A second stream, wet-ground mica, is reserved for the pearlescent paints used by the automotive industry.

The cosmetic industry draws on the same reflective and refractive properties, putting mica into blushes, eye shadow, eye liner, lipstick, mascara, and body glitter.

Drilling, plastics, and rubber take the rest. Well-drilling muds — the dense fluids pumped down a borehole to lift rock cuttings out — used 15 percent of dry-ground mica in 2008. The plastics industry adds it as an extender and filler, especially in automotive parts. The rubber industry uses it as an inert filler and as a mould-release compound, including in tyre manufacture.

Most sheet mica today comes from India, with smaller quantities from Russia and Madagascar. Indian and Madagascan mica is also mined artisanally, in poor working conditions and with the help of child labour.

Where it forms, where it's found

Geological setting

Muscovite is common in many different rock types as a primary mineral.

18,311recorded occurrences
Source · OpenStreetMap

Varieties

Physical

Hardness
123456789102.5/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Transparency
Transparent · Translucent
Colour
White to colorless · silvery-white · and tinged various colors by impurities.
Streak
White
Tenacity
elastic
Cleavage
Perfect

Perfect on (001).

Fracture
Micaceous
Density
2.77 g/cm³

Optical

Optical type
Biaxial (-) · 2V measured = 30 – 47° · 2V calc = 38 – 42°
Refractive index
1.552 – 1.618
Surface relief
Moderate
Principal indices
nα 1.552 – 1.576 · nβ 1.582 – 1.615 · nγ 1.587 – 1.618
Pleochroism
Weak

Weak when colored

Dispersion
r > v weak
Extinction
Z = b; X ∧ c = 0°-5°; Y ∧ a = 1°-3°.
Notes

Absorption: Faint, Y ≃ Z > X.

Michel-Lévy diagramhighlighted lineδ = 0.0385
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]385 nm1st order
Δ = 0Δmax
Thin-section mosaic70 grains · random 3D orientations
PPLpleochroism per grain
XPLindependent extinctions · rotate the stage
Interference simulatorsingle grain · PPL ↔ XPL
PPLpleochroism only · colour blends on rotation
XPLinterference colour · extinct every 90°
Retardation385 nm
Order1st order
XPL colour

Crystallography

Crystal system
Monoclinic
Space group
#10
Cell parameters
a = 5.199 Å · b = 9.027 Å · c = 20.106 Å
Cell angles
β = 95.78 °
Ratio a:b:c
1 : 1.736 : 3.867
Z
4
Morphology

Crystals uncommon, tabular (001) with rhombic to hexagonal outlines, often bound by (221), (111) and (010) (hkl refer to <f>-2M^1</f> polytype). Less common as prismatic, parallel to [001], with a crude hexagonal cross section. Most typically found as "books" and as flaky grains in various rocks. Sometimes in plumose or fibrous aggregates.

Twinning

Mica law twins common [310] forming six pointed stars, less common with the composition plane perpendicular to (001) (hkl refer to <f>-2M^1</f> polytype).

Parting
On (110) and (010).
Comment

Several monoclinic and triclinic polytypes are known. Cell data given for the <f>-2M^1</f> polytype (space group C2/c).

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen1215.999191.988
48.20%
14SiSiliconSilicon328.08584.255
21.15%
13AlAluminiumAluminium326.98280.946
20.32%
19KPotassiumPotassium139.09839.098
9.82%
1HHydrogenHydrogen21.0082.016
0.51%
Total398.303100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Impurities
  • Cr
  • Li
  • Fe
  • V
  • Mn
  • Na
  • Cs
  • Rb
  • Ca
  • Mg
  • H2O

Synonyms

  • Ammochrysos
  • Amphilogite
  • Antonit
  • Antonita
  • Antonite
  • Argent des chats
  • Astrolit
  • Astrolita
  • Didymite
  • Kaliglimmer
  • Katzensilber
  • Muscovy Glass
  • Muscowit
  • Muscowitow
  • Oncosine

In other languages

French
Alurgite · Ammochryse · Ammochrysos · Amphilogite · Antonite · Argent de chat · Argent des chats · Didymite · Mica argentin · Muscovite · Oncosine · Polychroïlite · Verre de Moscou
German
Hellglimmer · Katzensilber · Mariposit · Muskovit · Serizit · Tonerdeglimmer
Spanish
alurgita · mica blanca · moscovita
Italian
Moscovite · Muscovite
Portuguese
moscovita · Moscovite · Muscovita
Japanese
白雲母
Chinese
白雲母
Simplified Chinese
白云母
Traditional Chinese
白雲母
Russian
мусковит · Слюда-мусковита
Arabic
مسكوفيت

Classification

Strunz
10th ed.

9.EC.15

  • 9SilicatesClass
  • 9.EPhyllosilicatesDivision
  • 9.ECPhyllosilicates with mica sheets, composed of tetrahedral and octahedral netsGroup
  • 9.EC.15MuscoviteSpecies
Dana
8th ed.

71.02.2a.01

  • 71Phyllosilicates Sheets of Six-membered RingsClass
  • 71.02Sheets of 6-membered rings with 2:1 layersType
  • 71.02.2a— unnamed intermediate level —Group
  • 71.02.2a.01MuscoviteSpecies
CIM

16.3.8

  • 16Silicates Containing Aluminum and other MetalsClass
  • 16.3Aluminosilicates of KGroup
  • 16.3.8MuscoviteSpecies

Group, growth & confusion

In the same group
6 members
Commonly confused with
1 mineral

Literature, links & citation

Citations
  1. 1900Baumhauer, H. (1900) Ueber die Krystallformen des Muscovit. Zeitschrift für Kristallographie, 32 (1-6). 164-176 doi:10.1524/zkri.1900.32.1.164DOI: 10.1524/zkri.1900.32.1.164
  2. 1913Baumhauer, H. (1913) Über den Krystallbau der Lithionglimmer und die Verwachsung von Lepidolith und Muscovit. Zeitschrift für Krystallographie, 51 (1-6). 344-357 doi:10.1524/zkri.1913.51.1.344DOI: 10.1524/zkri.1913.51.1.344
  3. 1939Volk, Garth W. (1939) Optical and chemical studies of muscovite. American Mineralogist, 24 (4) 255-266
  4. 1939Gruner, John W. (1939) Formation and stability of muscovite in acid solutions at elevated temperatures. American Mineralogist, 24 (10) 624-628
  5. 1951Woodard, H.H. (1951) The Geology and Paragenesis of the Lord Hill pegmatite, Stoneham, Maine. American Mineralogist: 36: 869-883.
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Muscovite — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/muscovite-2815},
  note      = {Accessed 2026-05-11}
}