
mineral
Biotite on Quartz
Biotite Mica (K(Mg,Fe)3AlSi3O10(F,OH)2)
Hardness: 2.5-3.0 (Mohs). Color: Black, dark brown. Luster: Vitreous to pearly. Crystal Structure: Monoclinic (often tabular or platy). Cleavage: Perfect basal cleavage, allowing it to be peeled into thin sheets. Specific Gravity: 2.7-3.3.
- Hardness
- 2
- Color
- Black, dark brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5-3.0 (Mohs). Color: Black, dark brown. Luster: Vitreous to pearly. Crystal Structure: Monoclinic (often tabular or platy). Cleavage: Perfect basal cleavage, allowing it to be peeled into thin sheets. Specific Gravity: 2.7-3.3.
Formation & geological history
Commonly forms in metamorphic rocks such as schist and gneiss, and in igneous rocks like granite. It forms across a wide range of geological ages in high-temperature, high-pressure environments.
Uses & applications
Used as an insulating material in the electronics and electrical industries due to its thermal stability. It is also used as a filler in paints and as a component in drilling mud. Some specimens are kept by collectors for educational or aesthetic value.
Geological facts
Biotite is often called black mica. It is part of a solid-solution series between phlogopite and annite. It contains significant amounts of iron and magnesium which give it its distinctive dark color unlike transparent muscovite.
Field identification & locations
Identify in the field by its dark color, metallic or pearly luster, and the ability to flake off paper-thin sheets with a fingernail or blade. Often found as small shiny black flecks in granite countertops.
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Mineral/Rock
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mineral