
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale. Color: Range of purple, green, yellow, and clear (this specimen appears purplish-tan). Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Perfect octahedral in four directions. Specific Gravity: 3.18.
- Hardness
- 4 on Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale. Color: Range of purple, green, yellow, and clear (this specimen appears purplish-tan). Luster: Vitreous (glassy). Crystal Structure: Isometric/Cubic. Cleavage: Perfect octahedral in four directions. Specific Gravity: 3.18.
Formation & geological history
Forms as a late-stage mineral in hydrothermal veins, often associated with metallic ores like lead and silver. It can also form in sedimentary rocks like limestone or through sublimation in volcanic environments.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, in high-performance telescope and camera lenses, and widely as a semi-precious gemstone and for ornamental carvings.
Geological facts
Fluorite is the origin of the term 'fluorescence' because many specimens glow under ultraviolet light. It is often referred to as 'the most colorful mineral in the world'.
Field identification & locations
Identified in the field by its relatively low hardness (can be scratched by a knife but not a copper penny) and its distinctive octahedral cleavage. Commonly found in China, Mexico, South Africa, and the Illinois-Kentucky fluorspar district in the USA.
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Mineral
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Mineral/Rock
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