
mineral
Fluorite
Calcium Fluoride (CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale. Color: Green, purple, blue, or colorless (translucent). Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Perfect octahedral. Specific Gravity: 3.0 to 3.25.
- Hardness
- 4 on Mohs scale
- Color
- Green, purple, blue, or colorless (translucent)
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale. Color: Green, purple, blue, or colorless (translucent). Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Perfect octahedral. Specific Gravity: 3.0 to 3.25.
Formation & geological history
Forms in hydrothermal veins, often associated with metallic ores like lead and silver. It crystallizes from hot cooling fluids deep within the Earth's crust across various geological ages.
Uses & applications
Used as a flux in steel making, in the production of hydrofluoric acid, in high-precision camera lenses, and widely as a decorative gemstone and collector specimen.
Geological facts
Fluorite was the first mineral researched for fluorescence, a phenomenon named after this mineral. It is often called 'the most colorful mineral in the world'.
Field identification & locations
Identifiable by its 4-way perfect cleavage that often forms octahedrons and its relative softness (can be scratched by a knife but not a copper penny). Common locations include China, Mexico, South Africa, and the USA (Illinois/Kentucky).
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