
mineral
Fluorite
Calcium fluoride (CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale; Color: Colorless, green, purple, blue, or yellow; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.1-3.2.
- Hardness
- 4 on Mohs scale
- Color
- Colorless, green, purple, blue, or yellow
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: Colorless, green, purple, blue, or yellow; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.1-3.2.
Formation & geological history
Typically formed in hydrothermal veins or as an accessory mineral in igneous rocks like granites. It often occurs in association with minerals like quartz, calcite, and galena.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, in high-performance telescopes and camera lenses (due to low dispersion), and as a popular ornamental and gemstone material.
Geological facts
Fluorite is often intensely fluorescent under UV light; the term 'fluorescence' was actually derived from this mineral. It is the index mineral for hardness level 4 on the Mohs scale.
Field identification & locations
Identified in the field by its hardness (scratched by a knife but not a copper penny) and its perfect four-directional cleavage which often results in octahedral fragments. Frequently found in China, Mexico, South Africa, and the USA (Illinois/Kentucky).
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