Rock Identifier
Fluorite Cleavage Octahedron (Fluorite (Calcium Fluoride, CaF2)) — mineral
mineral

Fluorite Cleavage Octahedron

Fluorite (Calcium Fluoride, CaF2)

Hardness: 4 on Mohs scale; Color: typically green, purple, or colorless; Luster: vitreous; Crystal Structure: cubic; Cleavage: perfect octahedral in four directions; Specific Gravity: 3.17 to 3.56.

Hardness
4 on Mohs scale
Color
typically green, purple, or colorless
Luster
vitreous
Identified More mineral
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Physical properties

Hardness: 4 on Mohs scale; Color: typically green, purple, or colorless; Luster: vitreous; Crystal Structure: cubic; Cleavage: perfect octahedral in four directions; Specific Gravity: 3.17 to 3.56.

Formation & geological history

Formed in hydrothermal veins, often associated with metallic ores like lead and silver. It crystallizes from hot aqueous solutions as they cool or react with surrounding rocks like limestone.

Uses & applications

Used as a flux in steel making, in the manufacture of hydrofluoric acid, and for specialized optical lenses. Beautiful specimens are prized by collectors and used for decorative carvings and jewelry.

Geological facts

Fluorite is the origin of the term 'fluorescence' because many specimens glow under UV light. It is often called 'the most colorful mineral in the world'.

Field identification & locations

Identified by its octahedral shape (when cleaved), relative softness (can be scratched by a knife but not a penny), and vitreous luster. Commonly found in China, Mexico, South Africa, and the USA (Illinois/Kentucky).