
mineral
Rainbow Fluorite
Fluorite (Calcium Fluoride, CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale. Color: Green, purple, blue, and clear banding. Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic (though here carved into a heart). Cleavage: Perfect octahedral.
- Hardness
- 4 on Mohs scale
- Color
- Green, purple, blue, and clear banding
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale. Color: Green, purple, blue, and clear banding. Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic (though here carved into a heart). Cleavage: Perfect octahedral.
Formation & geological history
Forms primarily through hydrothermal activity in veins where hot, mineral-rich fluids circulate through crustal rocks. It can be found in sedimentary, igneous, and metamorphic environments.
Uses & applications
Used in the manufacture of hydrofluoric acid, as a flux in steelmaking/smelting, in optical lenses, and widely for jewelry, carvings, and metaphysical collecting.
Geological facts
Fluorite was the original mineral used to describe the phenomenon of fluorescence, where a mineral glows under UV light. It is often called the most colorful mineral in the world.
Field identification & locations
Identified by its distinctive color banding, softness (can be scratched by a steel knife but not a copper penny), and octahedral cleavage. Common locations include China, Mexico, South Africa, and the USA (Illinois).
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