
mineral
Biotite (Black Mica)
Biotite - K(Mg,Fe)3(AlSi3O10)(OH)2
Hardness: 2.5–3.0 Mohs; 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 Mohs; 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 primarily in igneous and metamorphic rocks through high-temperature and pressure environments. Common in granite, schist, and gneiss; found across most geological eras where tectonic activity occurs.
Uses & applications
Used in industry as a filler in paints and plastics, as a lubricant, and in the manufacturing of rubber. Occasionally used as a mineral specimen for educational purposes, though less common in jewelry due to its fragility.
Geological facts
Biotite is known as 'black mica' and is a common component of the rock cycle. It is often used by scientists for potassium-argon dating of rocks because it contains high levels of potassium.
Field identification & locations
Identify in the field by its black color and ability to peel into flexible, elastic flakes with a fingernail. Found worldwide, particularly in mountainous regions containing granite and metamorphic basement rocks.
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