
mineral
Fluorite
Calcium fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: Green (in this specimen), can be purple, blue, or yellow; Luster: Vitreous; Crystal Structure: Isometric (cubic); Cleavage: Perfect octahedral; Specific Gravity: 3.18
- Hardness
- 4 on Mohs scale
- Color
- Green (in this specimen), can be purple, blue, or yellow
- Luster
- Vitreous
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Physical properties
Hardness: 4 on Mohs scale; Color: Green (in this specimen), can be purple, blue, or yellow; Luster: Vitreous; Crystal Structure: Isometric (cubic); Cleavage: Perfect octahedral; Specific Gravity: 3.18
Formation & geological history
Formed primarily in hydrothermal veins, often associated with metallic ores. It can also occur in various igneous and some sedimentary environments. It forms through precipitation from late-stage magmatic fluids.
Uses & applications
Used as a flux in steel making, in the production of hydrofluoric acid, in high-performance telescope and camera lenses, and widely as a decorative stone and gemstone.
Geological facts
Many specimens of fluorite fluoresce under ultraviolet light, a phenomenon named after the mineral itself. It is known as 'the most colorful mineral in the world'.
Field identification & locations
Identified by its distinctive 4 on the Mohs scale (softer than glass) and its perfect octahedral cleavage. Found commonly in China, Mexico, South Africa, and the USA (Illinois/Kentucky).
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Mineral/Rock
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mineral