
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: typically purple, green, or blue in light-colored hues; Luster: Vitreous; Crystal system: Isometric/Cubic; Cleavage: Perfect octahedral; Specific gravity: 3.17 to 3.56.
- Hardness
- 4 on Mohs scale
- Color
- typically purple, green, or blue in light-colored hues
- Luster
- Vitreous
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Physical properties
Hardness: 4 on Mohs scale; Color: typically purple, green, or blue in light-colored hues; Luster: Vitreous; Crystal system: Isometric/Cubic; Cleavage: Perfect octahedral; Specific gravity: 3.17 to 3.56.
Formation & geological history
Formed through hydrothermal activity in sedimentary or igneous environments. It often occurs as a gangue mineral in metal ores, particularly with lead and silver veins. Most specimens are from the Phanerozoic eon.
Uses & applications
Used as a flux in steel making, in the manufacture of opalescent glass, as an enamel for cooking utensils, and for hydrofluoric acid production. High-clear specimens are used in telescope optics. Very popular in gemstone carving and lapidary art.
Geological facts
Fluorite exhibits the property of fluorescence under UV light, a term which was actually named after this mineral. It is often referred to as 'The Most Colorful Mineral in the World'.
Field identification & locations
Identified by its octahedral cleavage planes and its relatively low hardness (can be scratched by a pocket knife). Commonly found in Mexico, China, and the United States (Illinois). Collectors should look for distinct crystalline faces.
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