
mineral
Fluorite on Matrix
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: Purple, green, and clear; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic); Cleavage: Perfect octahedral in four directions; Specific Gravity: 3.175 to 3.56.
- Hardness
- 4 on Mohs scale
- Color
- Purple, green, and clear
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: Purple, green, and clear; Luster: Vitreous (glassy); Crystal structure: Isometric (cubic); Cleavage: Perfect octahedral in four directions; Specific Gravity: 3.175 to 3.56.
Formation & geological history
Formed through hydrothermal activity, often in veins or as a gangue mineral in metallic ore deposits. This specimen appears to be from a sedimentary host rock origin, likely formed in a low-temperature hydrothermal environment.
Uses & applications
Used primarily as a flux in steel making, in the production of hydrofluoric acid, as a source of fluorine, and as a popular semi-precious gemstone for decorative carvings and jewelry.
Geological facts
Fluorite is the mineral from which the phenomenon of fluorescence was named, as many specimens glow strongly under ultraviolet light. It is often called the most colorful mineral in the world.
Field identification & locations
Identified by its octahedral cleavage, its relatively low hardness (can be scratched by a knife but not a penny), and its vibrant purple hues when associated with limestone or quartz matrix. Commonly found in Illinois (USA), China, and Mexico.
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