
mineral
Fluorite (Fluorescent)
Calcium Fluoride (CaF2)
Hardness: 4.0 on Mohs scale; Color: Variable (white in normal light, blue under UV); Luster: Vitreous; Crystal Structure: Isometric; Cleavage: Perfect octahedral
- Hardness
- 4
- Color
- Variable (white in normal light, blue under UV)
- Luster
- Vitreous
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Physical properties
Hardness: 4.0 on Mohs scale; Color: Variable (white in normal light, blue under UV); Luster: Vitreous; Crystal Structure: Isometric; Cleavage: Perfect octahedral
Formation & geological history
Hydrothermal origin, typically found in veins formed at low to moderate temperatures as minerals precipitate from hot, mineral-rich fluids. Found in limestone units.
Uses & applications
Used as a flux in steelmaking, in the production of hydrofluoric acid, high-fidelity camera lenses, and as a popular collector's mineral.
Geological facts
The phenomenon of 'fluorescence' was actually named after fluorite in 1852 by George Gabriel Stokes. Not all fluorite glows; the effect is usually caused by trace impurities like europium.
Field identification & locations
Identify by its perfect cleavage and specific blue glow under a UV lamp. Commonly found in Illinois, Kentucky, and widespread locations in China and Mexico.
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