What is Muscovite?
Muscovite is the most common mineral of the mica family. It is an important rock-forming mineral present in igneous,
metamorphic and sedimentary rocks. Like other micas it readily cleaves into thin transparent sheets. Muscovite
sheets have a pearly to vitreous luster on their surface. If they are held up to the light they are transparent and
nearly colorless, but most have a slight brown, yellow, green or rose-color tint.
The ability of muscovite to split into thin transparent sheets - sometimes up to several feet across - gave it an early
use as window panes. In the 1700s it was mined for this use from pegmatites in the area around Moscow, Russia. These
panes were called "muscovy glass" and that term is thought to have inspired the mineral name "muscovite".
Sheet muscovite is an excellent insulator and that makes it suitable for manufacturing specialized parts for electrical
equipment. Scrap, flake and ground muscovite are used as fillers and extenders in a variety of paints, surface treatments
and manufactured products. The pearlescent luster of muscovite makes it an important ingredient that adds "glitter" to
paints, ceramic glazes and cosmetics.
Muscovite is easily identified because its perfect cleavage allows it to be split into thin, flexible, elastic, colorless,
transparent sheets with a pearly to vitreous luster. It is the only common mineral with these properties.
Physical Properties of Muscovite
||thick specimens often appear to be black, brown or silver in color; however, when split into thin sheets muscovite is colorless, sometimes with a tint of brown, yellow, green, or rose
||white, often sheds tiny flakes
||pearly to vitreous
||transparent to translucent
||2.5 to 3
||2.8 to 2.9
||cleavage, color, transparency
||Used in the manufacturing of paint, joint compound, plastics rubber, asphalt roofing, cosmetics, drilling mud.
An Important Rock-Forming Mineral
Muscovite is found in igneous, metamorphic and sedimentary rocks. In igneous rocks it is a primary mineral that is
especially common in granitic rocks. In granite pegmatites muscovite is often found in large crystals with a
pseudohexagonal outline. These crystals are called "books" because they can be split into paper-thin sheets.
Muscovite rarely occurs in igneous rocks of intermediate, mafic and ultramafic composition.
Muscovite can form during the regional metamorphism of argillaceous rocks. The heat and pressure of metamorphism
transforms clay minerals into tiny grains of mica which enlarge as metamorphism progresses. Muscovite can occur as
isolated grains in schist and gneiss or it can be abundant enough that the rocks are called "mica schist" or "micaceous gneiss".
Muscovite is not especially resistant to chemical weathering. It is quickly transformed into clay minerals. Tiny flakes
of muscovite sometimes survive long enough to be incorporated into sediments and immature sedimentary rocks. It is evidence
that these sediments and rocks have not been subjected to severe weathering.
Muscovite is a potassium-rich mica with the following generalized composition...
In this formula potassium is sometimes replaced by other ions with a single positive charge such as sodium, rubidium or
cesium. Aluminum is sometimes replaced by magnesium, iron, lithium, chromium or vanadium.
Uses of Ground Mica
Ground mica, mostly muscovite, is used in the United States to manufacture a variety of products .
The primary use of ground mica is in joint compound used to finish seams and blemishes in gypsum wallboard. The mica serves
as a filler, improves the workability of the compound and reduces cracking in the finished product. In 2011 about 69%
of the dry-ground mica consumed in the United States was used in joint compound.
Ground mica is used as a pigment extender in paint. It helps keep pigment in suspension; reduces chalking, shrinking and
shearing of finished surface; reduces water penetration and weathering and brightens the tone of colored pigments. In
some automotive paints tiny flakes of mica are used to produce a pearlescent luster.
Ground mica is an additive to drilling mud that helps to seal porous sections of the drill hole to reduce circulation loss.
In 2011, about 17% of the dry-ground mica consumed in the United States was used in drilling muds.
The auto industry in the United States uses ground mica to improve the performance of plastic parts. In plastics, particles
of ground mica serve as an agent to absorb sound and vibration. It can also improve mechanical properties by increasing
stability, stiffness and strength.
Ground mica is used as an inert filler and mold release agent in the manufacture of molded rubber products such as tires
and roofing. The platy grains if mica act as an antisticking agent.
Dry-ground mica is used as a surface coating on asphalt shingles and rolled roofing. The flat mica particles coat the
surface and act as an antistick agent. The mica does not absorb the asphalt and stands up well to weathering.
Some of the highest quality ground mica is used in the cosmetics industry. The pearly luster of ground mica makes it
an important ingredient in blushes, eyeliner, eye shadow, foundation, hair and body glitter, lipstick, lip gloss, mascara,
and nail polish.
Uses of Sheet Mica
While ground mica might sell for $300 per metric ton, sheet mica for specialty uses can sell for prices up to $2000 per
kilogram. Mica has several properties that make it suitable for very special uses:
1) it can be split into thin sheets
2) the sheets are chemically inert, dielectric, elastic, flexible, hydrophilic, insulating, lightweight, reflective, refractive and resilient
3) it is stable when exposed to electricity, light, moisture and extreme temperatures
Most sheet mica is used to make electronic devices. In these uses the sheets are cut, punched, stamped and machined to
precision dimensions. Uses include: diaphragms for oxygen breathing equipment, marker dials for navigation compasses,
optical filters, pyrometers, retardation plates in helium-neon lasers, missile systems components, medical electronics,
optical instrumentation, radar systems, radiation detector windows, and calibrated capacitors.
The quality of sheet mica is influenced by the presence of inclusions. These can impair splitting, decrease transparency,
and reduce dielectric strength. Tiny crystals of staurolite, zircon, garnet, tourmaline, magnetite, hematite and other
minerals can form between the sheets and orient parallel to the mica's crystal structure. Inclusions decrease the mica's
value and its ability to be used in most applications.
(See image at right.)
The use of ground mica is mainly determined by activity levels of the construction and auto industries. An increase in
domestic oil and gas drilling should sustain the demand for mica additives for drilling mud. Producers in the United States
should be able to supply domestic demand with some mica being imported for specialty use or where transportation from
domestic producers to the consumer is more costly than imported mica. About 50,000 tons was produced in the United States
in 2011 with about 25,000 tons being imported. China at 700,000 tons, is the largest producer and largest consumer.
Although the demand for sheet mica is growing with the advance of technology the prices are so high that the invention of
substitute materials is growing. Some of these involve making mica sheets from ground mica composites or the creation of synthetic micas in
laboratories. Acrylic, fiberglass, nylatron, nylon, polyester, styrene, vinyl-PVC and vulcanized fibers are all finding use
as sheet mica substitutes .
 Mica: Jason Christopher Willett, 2011 Minerals Yearbook, United States Geological Survey, September 2012.
 Mica (Natural): Jason Christopher Willett, 2013 Mineral Commodity Summary, United States Geological Survey, January, 2013.
Contributor: Hobart King
Find it on Geology.com
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|Bladed muscovite from the Nurestan Province of Afghanistan with a crystal of pink morganite beryl. Specimen is approximately 2 1/4 x 2 x 1 1/2 inches (5.9 x 4.8 x 3.4 centimeters). Photograph by Rob Lavinsky, iRocks.com, Creative Commons License: CC-BY-SA-3.0.
|Muscovite from Stoneham, Maine. Specimen is approximately 4 inches (10 centimeters) across. Hand specimens of this size and thickness often appear to have a black, brown or silver color; however, when they are split into thin sheets the clear transparent nature of muscovite is revealed. Thin sheets often have a slight tint of brown, green, yellow or rose.
|A specimen of muscovite schist. Muscovite is formed during the metamorphism of argillaceous rocks. specimen shown is about two inches (five centimeters) across.
|Muscovite from Mitchell County, North Carolina. Specimen is approximately 3 inches (7.6 centimeters) across.
|Muscovite from Mitchell County, North Carolina. Specimen is approximately 3 inches (7.6 centimeters) across. The transparent nature of muscovite is clearly seen in this photo.
|Photograph of ground muscovite from Mt. Turner, Australia. USGS image.
|Mica is heat resistant and is often used as a "window" for wood stoves, ovens and furnaces. These mica windows are for a wood stove and are about the same thickness as a piece of paper. Sheet size is 3 inches x 4 inches. They can be trimmed with scissors to fit the size of the window.
|Sheets of mica with inclusions are often sold as low quality windows for woodstoves, ovens and furnaces at a reduced price. Common inclusions are magnatite, rutile and hematite. Sheet size is 6 inches x 6 inches.