
mineral
Fluorite Geode
Calcium Fluoride (CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale; Color: typically green, purple, or colorless as seen here; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.18.
- Hardness
- 4 on Mohs scale
- Color
- typically green, purple, or colorless as seen here
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: typically green, purple, or colorless as seen here; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.18.
Formation & geological history
Formed in hydrothermal veins and cavities when hot, mineral-rich fluids circulate through host rock. This specimen appears to be a vug or geode-like cavity filling, likely from a sedimentary or hydrothermal environment.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, in high-performance telescope and camera lenses, and as decorative cabinet specimens.
Geological facts
Fluorite is the most common mineral used to define the hardness of 4 on the Mohs scale. Some specimens exhibit strong fluorescence under UV light, a property named after the mineral itself.
Field identification & locations
Identify by its 4-directional cleavage and relatively low hardness (can be scratched by a knife but not a penny). Look for it in limestone or hydrothermal ore veins across locations like Illinois (USA), Mexico, and China.
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