
mineral
Green Fluorite
Fluorite (Calcium Fluoride, CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale; Color: Pale green (translucent); Luster: Vitreous (glassy); Crystal structure: Isometric (cubic or octahedral cleavage); Cleavage: Perfect octahedral in four directions; Specific Gravity: 3.18
- Hardness
- 4 on Mohs scale
- Color
- Pale green (translucent)
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: Pale green (translucent); Luster: Vitreous (glassy); Crystal structure: Isometric (cubic or octahedral cleavage); Cleavage: Perfect octahedral in four directions; Specific Gravity: 3.18
Formation & geological history
Formed through hydrothermal activity where hot, fluorine-rich fluids circulate through host rocks like limestone or granite. It is commonly found in veins or as a gangue mineral in metallic ore deposits.
Uses & applications
Industrial uses include acting as a flux for smelting steel (smelting and refining), the manufacture of hydrofluoric acid, and high-quality optical lenses. It is also popular in decorative carvings and jewelry.
Geological facts
Fluorite gave its name to the phenomenon of 'fluorescence' because many specimens glow under ultraviolet light. It is often referred to as 'the most colorful mineral in the world'.
Field identification & locations
Identify in the field by its 4-way octahedral cleavage, its ability to be scratched by a steel knife but not a copper penny, and its glassy luster. Common locations include China, Mexico, South Africa, and Illinois, USA.
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