Chemical Formula |
KAl3Si3O10(OH)2 |
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Composition |
Basic potassium aluminum silicate, sometimes with some chromium or manganese replacing the aluminum |
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Variable Formula |
K(Al,Cr,Mn)3Si3O10(OH)2 |
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Color |
Colorless, white, beige, yellow, brown, gray, green, pink, purple, red, black; occasionally multicolored |
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Streak |
Colorless |
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Hardness |
2 - 2.5 |
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Crystal System |
Monoclinic |
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Crystal Forms |
Crystals are in thick flakes, micaceous masses and groupings, and in tabular, foliated, flaky, and scaly forms. Crystals may also be elongated with one dimension flat, or stubby triangular or hexagonally shaped crystals. Muscovite also forms interesting aggregates of dense bladed crystals, thick rosettes, uniquely twinned star-shaped formations, and rounded botryoidal and globularmasses of dense flakes. |
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Transparency |
Transparent to translucent |
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Specific Gravity |
2.7 - 3.0 |
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Luster |
Pearly |
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Cleavage |
1,1 |
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Fracture |
Uneven |
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Tenacity |
Sectile, Elastic |
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Other ID Marks |
Tendency for small pieces or flakes or peel off. |
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In Group |
Silicates; Phyllosilicates; Mica Group |
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Striking Features |
Flaky habit, crystals, sectility, and mode of occurence. |
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Environment |
Muscovite is a very common rock-forming mineral and is an important constituent in many environments. Its presence is noted especially in granite pegmatites, in contact metamorphic rocks, in metamorphic schists, and in hydrothermal veins. Important Muscovite deposits where large significant crystals occur are almost exclusively from granite pegmatites. |
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Rock Type |
Igneous, Metamorphic |
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Popularity (1-4) |
1 |
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Prevalence (1-3) |
1 |
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Demand (1-3) |
1 |
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