
mineral
Fluorite on Matrix
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale. Color: Pale translucent green to yellowish-grey embedded crystal. Luster: Vitreous to sub-vitreous. Cleavage: Perfect isometric/octahedral cleavage evident in cracked sections.
- Hardness
- 4 on Mohs scale
- Color
- Pale translucent green to yellowish-grey embedded crystal
- Luster
- Vitreous to sub-vitreous
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Physical properties
Hardness: 4 on Mohs scale. Color: Pale translucent green to yellowish-grey embedded crystal. Luster: Vitreous to sub-vitreous. Cleavage: Perfect isometric/octahedral cleavage evident in cracked sections.
Formation & geological history
Formed via hydrothermal activity where fluorine-bearing fluids permeate host rock fractures and cavities, precipitating fluorite alongside quartz and calcite minerals.
Uses & applications
Fluorite is used as a flux in steelmaking, in the production of hydrofluoric acid, in high-performance optical lenses, and as a popular collectible mineral specimen.
Geological facts
Fluorite gave its name to the phenomenon of fluorescence because many specimens glow under ultraviolet light due to trace element impurities like europium.
Field identification & locations
Identified by its cubic crystal habits, perfect cleavage, soft hardness (can be scratched by steel), and frequent association with hydrothermal quartz matrix. Common in England, China, Mexico, and USA.
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