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MUSCOVITE MICA 
BY- ASHISH RANJAN, 12411008
What is Mica? 
 Mica is a generic term applied to a group of rock-forming complex 
aluminosilicate minerals having a sheet or plate like structure with varying 
chemical composition and physical properties.
Types Of Mica 
Of the nine common varieties in the mica group of minerals, the two principal 
classes of Mica types of commercial importance are 
 Muscovite : K Al2 (Al Si3 O10 )(OH) 2 and 
 Phlogopite : K Mg3 (Al Si3O10 )(OH) 2
Muscovite Mica 
 It is a hydrous potassium aluminium silicate with a predominance of 
potassium. It ranges from colourless through browns to greens or reds.
Phlogopite Mica 
 It is a hydrous magnesium aluminium silicate with a predominance of 
magnesium. It is commonly called as “Amber Mica” which varies in colour 
from light silver to dark brown or amber.
Occurence 
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.
 Exploration and exploitation is successfully carried 
by means of systematic vertical shaft and open cast 
mining. The principal muscovite mica deposits are 
chiefly found in the States of Jharkhand, Rajasthan 
and Andhra Pradesh. 
 Jharkhand (formerly Bihar State) which produces the 
world's finest muscovite mica well known throughout 
the globe
Muscovite 
Mica may be 
divided into two 
color groups : 
RUBY MUSCOVITE 
GREEN MUSCOVITE
Ruby Muscovite 
Colour ranges from an almost white 
through pink to a light ruby and 
into shades of brownish ruby and 
brown. It is produced in the Indian 
States of Jharkhand and Rajasthan.
Green Muscovite 
Ranges from light to pale green through yellowish 
and olive green to a dark green. It is produced 
in the Indian State of Andhra Pradesh.
Physical Properties 
 Lustre -Vitreous, Silky, Pearly 
 Diaphaneity (Transparency):Transparent, 
Translucent
 Colour:White to colorless, silvery-white, and tinged various colors by 
impurities. 
 Streak:White 
 Hardness (Mohs): 2½
 Cleavage:Perfect 
Perfect on {001}. 
 Fracture:Micaceous 
 Crystal System: Monoclinic with 
a = 5.199Å, b = 9.027Å, c = 20.106Å 
β = 95.78°
DISTINGUISHING SIMILAR MINERALS 
 Chlorite and Margarite - Not as elastic as Muscovite. 
 Biotite, Phlogopite - Usually darker in color, otherwise very difficult to 
distinguish. 
 Lepidolite - Very difficult to distinguish from pink Muscovite. 
 Gypsum - Cannot be peeled into micaceous sheets, crystals usually 
differently shaped.
Uses
THANK YOU
 Muscovite is an extremely common mineral, some bright yellow and others with perfect 
star formations, come from the famous pegmatite localites in the Doce and 
Jequitinhonha Valleys in Minas Gerais Brazil. Specific localities include Divino das 
Laranjeiras ("stars"),Galileia, Governador Valadares, Conselheiro Pena, Jaguaracu, 
Aracuai, and Coronel Murta. Beautiful yellow Muscovite comes from the Davib Ost Farm, 
Karibib, Erongo, Namibia. Fine Muscovite plates, often associated with 
valuable pegmatitegemstones, come from the Shigar Valley and Skardu District in 
Northern Pakistan. Nellore, India, is famous for its Muscovite mines which have produced 
some of the worlds largest mica sheets. Xuebaoding Mountain, Pingwu, in Sichuan 
Province, China, provides excellent Aquamarine and Scheelite that are associated with 
beautiful Muscovite plates. 
In the U.S., Muscovite is fairly common in the pegmatites of San Diego county, including 
Pala and Ramona. Rare Muscovitepseudomorphs after Tourmaline come from the Willow 
Spring Ranch, Oracle, Pinal Co., Arizona. A bright pink, lithium-rich variety comes from the 
Harding Mine, Taos Co., New Mexico; and gemmy green crystals from Lincoln Co., North 
Carolina. Other important localties include Mt Antero, Chaffee Co., Colorado; the 
Diamond Mica Mine, Keystone, Pennington Co., South Dakota; Shelby, Cleveland Co., 
North Carolina; and Bedford, Westchester Co., New York. 
New England contains some important Muscovite in its famous pegmatites, specifically at 
Middlesex Co., Connecticut (East Hampton, Haddam, and Portland); Grafton Co., New 
Hampshire (the Palermo No. 1 Mine, Groton; and the Ruggles Mine, Grafton); Mt. Apatite, 
Auburn, Androscoggin Co., Maine; and Greenwood and Newry, Oxford Co., Maine.

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Muscovite Mica Properties

  • 1. MUSCOVITE MICA BY- ASHISH RANJAN, 12411008
  • 2. What is Mica?  Mica is a generic term applied to a group of rock-forming complex aluminosilicate minerals having a sheet or plate like structure with varying chemical composition and physical properties.
  • 3. Types Of Mica Of the nine common varieties in the mica group of minerals, the two principal classes of Mica types of commercial importance are  Muscovite : K Al2 (Al Si3 O10 )(OH) 2 and  Phlogopite : K Mg3 (Al Si3O10 )(OH) 2
  • 4. Muscovite Mica  It is a hydrous potassium aluminium silicate with a predominance of potassium. It ranges from colourless through browns to greens or reds.
  • 5. Phlogopite Mica  It is a hydrous magnesium aluminium silicate with a predominance of magnesium. It is commonly called as “Amber Mica” which varies in colour from light silver to dark brown or amber.
  • 6. Occurence 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.
  • 7.  Exploration and exploitation is successfully carried by means of systematic vertical shaft and open cast mining. The principal muscovite mica deposits are chiefly found in the States of Jharkhand, Rajasthan and Andhra Pradesh.  Jharkhand (formerly Bihar State) which produces the world's finest muscovite mica well known throughout the globe
  • 8.
  • 9.
  • 10. Muscovite Mica may be divided into two color groups : RUBY MUSCOVITE GREEN MUSCOVITE
  • 11. Ruby Muscovite Colour ranges from an almost white through pink to a light ruby and into shades of brownish ruby and brown. It is produced in the Indian States of Jharkhand and Rajasthan.
  • 12. Green Muscovite Ranges from light to pale green through yellowish and olive green to a dark green. It is produced in the Indian State of Andhra Pradesh.
  • 13. Physical Properties  Lustre -Vitreous, Silky, Pearly  Diaphaneity (Transparency):Transparent, Translucent
  • 14.  Colour:White to colorless, silvery-white, and tinged various colors by impurities.  Streak:White  Hardness (Mohs): 2½
  • 15.  Cleavage:Perfect Perfect on {001}.  Fracture:Micaceous  Crystal System: Monoclinic with a = 5.199Å, b = 9.027Å, c = 20.106Å β = 95.78°
  • 16. DISTINGUISHING SIMILAR MINERALS  Chlorite and Margarite - Not as elastic as Muscovite.  Biotite, Phlogopite - Usually darker in color, otherwise very difficult to distinguish.  Lepidolite - Very difficult to distinguish from pink Muscovite.  Gypsum - Cannot be peeled into micaceous sheets, crystals usually differently shaped.
  • 17. Uses
  • 18.
  • 19.
  • 20.
  • 22.  Muscovite is an extremely common mineral, some bright yellow and others with perfect star formations, come from the famous pegmatite localites in the Doce and Jequitinhonha Valleys in Minas Gerais Brazil. Specific localities include Divino das Laranjeiras ("stars"),Galileia, Governador Valadares, Conselheiro Pena, Jaguaracu, Aracuai, and Coronel Murta. Beautiful yellow Muscovite comes from the Davib Ost Farm, Karibib, Erongo, Namibia. Fine Muscovite plates, often associated with valuable pegmatitegemstones, come from the Shigar Valley and Skardu District in Northern Pakistan. Nellore, India, is famous for its Muscovite mines which have produced some of the worlds largest mica sheets. Xuebaoding Mountain, Pingwu, in Sichuan Province, China, provides excellent Aquamarine and Scheelite that are associated with beautiful Muscovite plates. In the U.S., Muscovite is fairly common in the pegmatites of San Diego county, including Pala and Ramona. Rare Muscovitepseudomorphs after Tourmaline come from the Willow Spring Ranch, Oracle, Pinal Co., Arizona. A bright pink, lithium-rich variety comes from the Harding Mine, Taos Co., New Mexico; and gemmy green crystals from Lincoln Co., North Carolina. Other important localties include Mt Antero, Chaffee Co., Colorado; the Diamond Mica Mine, Keystone, Pennington Co., South Dakota; Shelby, Cleveland Co., North Carolina; and Bedford, Westchester Co., New York. New England contains some important Muscovite in its famous pegmatites, specifically at Middlesex Co., Connecticut (East Hampton, Haddam, and Portland); Grafton Co., New Hampshire (the Palermo No. 1 Mine, Groton; and the Ruggles Mine, Grafton); Mt. Apatite, Auburn, Androscoggin Co., Maine; and Greenwood and Newry, Oxford Co., Maine.

Editor's Notes

  1. Crystals of Mica are characterised by highly perfect basal cleavage in the direction of large surfaces permitting it to split or delaminate into extremely thin and flat films. 
  2. Types of Mica Anandite, Annite, Biotite, Celadonite, Roscoelite, Illite Phlogopite from Kiran, Kokcha Valley, Badakhshan, Afghanistan Lazurite
  3.  Muscovy Glass, Cat Silver, and Lapis Specularis (stone mirror); The name muscovite comes from Muscovy-glass, a name given to the mineral in Elizabethan England due to its use in medieval Russia as a cheaper alternative to glass in windows.  Muscovite Mica is transparent and harder than Phlogopite Mica having more widespread availability. Muscovite Mica from Bancroft, Ontario CANADA
  4. Transparency is less than Muscovite Mica and its films are a bit cloudy. Phlogopite Mica is softer than Muscovite Mica but has greater heat resistance and thermal durability.
  5. 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". Sheets of muscovite 5×3 m have been found in Nellore, India. A pegmatite is a holocrystalline, intrusive igneous rock composed of interlocking phaneritic crystals usually larger than 2.5 cm in size; such rocks are referred to aspegmatitic. Most pegmatites are composed of quartz, feldspar and mica, having a similar basic composition as granite.
  6. COMMON MINERAL ASSOCIATIONS - Albite, Quartz, Microcline, Almandine, Spodumene "argillaceous" is also used to define rocks in which clay minerals are a secondary but significant component.  Vast exploitable reserves are found chiefly in India which produces and markets over 80% of the total global output of Muscovite Mica.
  7. The green, chromium-rich variety is called fuchsite; (mariposite)- cr rich Both Ruby Mica and Green Mica are equally suitable under normal working conditions. Fuschite, Alurgite, Mariposite, Schernikite , Sericite, Star Muscovite 
  8. Still, Ruby Mica is generally preferred since at elevated temperatures Green Mica displays erratic electrical characteristics. The structure of Green Muscovite is stable but less perfect as compared to Ruby Muscovite. Moreover, Ruby Muscovite is harder than Green Muscovite having excellent cleavage permitting it to be split into the thinnest desired film without the risk of cracking.
  9. It is a Phylosilicates minerals, i.e they have each set of tetrahedrons surrounded by three oxygen atoms, forming a sheet like structure.
  10. Crystals are in thick flakes, micaceous masses and groupings, and in tabular, foliated, flaky, and scalyforms.
  11. Tenacity:Elastic It has a highly-perfect basal cleavage yielding remarkably-thin laminæ (sheets) which are often highly elastic.
  12. Muscovite is in demand for the manufacture of fireproofing and insulating materials and to some extent as a lubricant.