
mineral
Biotite / Black Mica
Biotite K(Mg,Fe)3AlSi3O10(F,OH)2
Hardness: 2.5 - 3.0 on Mohs scale; Color: Black, dark green, or dark brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.7 - 3.3.
- Hardness
- 2
- Color
- Black, dark green, or dark brown
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2.5 - 3.0 on Mohs scale; Color: Black, dark green, or dark brown; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect basal (peels into thin sheets); Specific Gravity: 2.7 - 3.3.
Formation & geological history
Formed in a wide range of geological conditions; commonly found in igneous rocks like granite and pegmatites, as well as metamorphic rocks like schist and gneiss. It can also form through hydrothermal processes.
Uses & applications
Used historically as an insulator in electrical equipment and as a filler in paints and rubber. Its main value today is in geological research and as a collector's specimen.
Geological facts
Biotite is known as 'black mica' and is part of the mica group. It is unusual because it can contain radioactive elements like potassium-40, making it useful for dating the age of rocks through potassium-argon dating.
Field identification & locations
Identify in the field by its dark color and the way it flakes into flexible, elastic thin sheets (mica books). It is commonly found in mountainous regions globally, particularly in pegmatite veins.
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