
mineral
Biotite (Mica)
Biotite group (K(Mg,Fe)3AlSi3O10(F,OH)2)
Hardness: 2.5-3.0 Mohs; Color: Black, dark brown, or dark green; Luster: Pearly to vitreous; Crystal Structure: Monoclinic (pseudo-hexagonal); Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.7-3.3
- Hardness
- 2
- Color
- Black, dark brown, or dark green
- Luster
- Pearly to vitreous
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Physical properties
Hardness: 2.5-3.0 Mohs; Color: Black, dark brown, or dark green; Luster: Pearly to vitreous; Crystal Structure: Monoclinic (pseudo-hexagonal); Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.7-3.3
Formation & geological history
Forms in a wide range of geological environments, primarily igneous rocks like granite and metamorphic rocks like schist and gneiss. It is a common rock-forming mineral formed through the cooling of magma or the metamorphism of clay-rich sedimentary rocks.
Uses & applications
Used as an insulating material in the electrical industry (due to heat and electrical resistance), as a filler in paints and rubber, and as an additive in drilling mud. It is also highly valued as a geological specimen for students and collectors.
Geological facts
Biotite is often referred to as 'black mica' and is part of the phyllosilicate mineral group. It is a key index mineral used by geologists to determine the temperature and pressure history of metamorphic rocks. Unlike muscovite, it is rarely transparent when in thick books.
Field identification & locations
Identify in the field by its dark color and 'books' of thin, flexible, elastic sheets that can be peeled away with a fingernail. It is common in the Appalachian Mountains, Scandinavia, and Canada. Collectors look for large, intact 'books' or crystals showing well-defined hexagonal outlines.
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