
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on the Mohs scale. Color: Highly variable, commonly purple, green, blue, yellow, or clear. Luster: Vitreous to sub-vitreous. Crystal Structure: Isometric (cubic). Cleavage: Perfect octahedral cleavage in four directions. Specific gravity: 3.18.
- Hardness
- 4 on the Mohs scale
- Luster
- Vitreous to sub-vitreous
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Physical properties
Hardness: 4 on the Mohs scale. Color: Highly variable, commonly purple, green, blue, yellow, or clear. Luster: Vitreous to sub-vitreous. Crystal Structure: Isometric (cubic). Cleavage: Perfect octahedral cleavage in four directions. Specific gravity: 3.18.
Formation & geological history
Forms in hydrothermal veins, often associated with metallic ores like lead and zinc, as well as in cavities in limestone and dolomite. Geological age varies widely depending on the deposit.
Uses & applications
Used in metallurgy as a flux, in the manufacture of opalescent glass, enamels, and hydrofluoric acid, as well as in optical equipment, carvings, and collector gemstones.
Geological facts
Fluorite is the defining mineral for a hardness of 4 on the Mohs scale. It gave the term 'fluorescence' its name because many specimens glow strongly under ultraviolet light due to impurities like yttrium.
Field identification & locations
Identified by its relatively low hardness (easily scratched with a knife but not a copper coin), perfect octahedral cleavage, and often vibrant purple or green coloring. Found worldwide, with major deposits in China, Mexico, South Africa, and the USA.
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