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.
Muscovite may also form pseudomorphs after other minerals, assuming the original minerals crystal shape.
Transparency
Transparent to translucent
Specific Gravity
2.7 - 3.0
Luster
Pearly
Cleavage
1,1
Fracture
Uneven
Tenacity
Sectile, Elastic
Other ID Marks
Tendency for small pieces or flakes or peel off.
In Group
Silicates; Phyllosilicates; Mica Group
Striking Features
Flaky habit, crystals, sectility, and mode of occurence.
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.
Rock Type
Igneous, Metamorphic
Popularity (1-4)
1
Prevalence (1-3)
1
Demand (1-3)
1
OTHER NAMES
Common Mica
Isinglass
Old name for mica, especially Muscovite. May also describe mica in the form of large, thin sheets.