
mineral
Green Fluorite
Fluorite (Calcium Fluoride, CaF2)
AI-generated identification · may be incorrectHardness: 4 (Mohs scale); Color: Mint to emerald green; Luster: Vitreous (glassy); Crystal structure: Isometric (often cubic or octahedral); Cleavage: Perfect octahedral in four directions; Specific gravity: 3.1
- Hardness
- 4 (Mohs scale)
- Color
- Mint to emerald green
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 (Mohs scale); Color: Mint to emerald green; Luster: Vitreous (glassy); Crystal structure: Isometric (often cubic or octahedral); Cleavage: Perfect octahedral in four directions; Specific gravity: 3.1
Formation & geological history
Formed through hydrothermal activity, often in veins or as a gangue mineral in metallic ore deposits. It occurs in various geological environments from volcanic settings to sedimentary limestone basins.
Uses & applications
Used as a flux in steel making, in the manufacture of opalescent glass, and as a source of fluorine for hydrofluoric acid. High-quality specimens are used in jewelry (as beads or cabochons) and as decorative collectibles.
Geological facts
Fluorite is the origin of the term 'fluorescence' because many specimens glow under ultraviolet light. It is often called 'the most colorful mineral in the world'.
Field identification & locations
Identify in the field by its distinct green color, glassy luster, and relatively low hardness (can be scratched by a steel knife). Look for its characteristic four directions of perfect cleavage.
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