
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: typically purple, green, yellow, or colorless in this specimen; Luster: vitreous (glassy); Crystal structure: Isometric (cubic); Cleavage: Perfect octahedral; Specific gravity: 3.175 to 3.56.
- Hardness
- 4 on Mohs scale
- Luster
- vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: typically purple, green, yellow, or colorless in this specimen; Luster: vitreous (glassy); Crystal structure: Isometric (cubic); Cleavage: Perfect octahedral; 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. It can also occur in sedimentary rocks like limestone and in some igneous environments such as pegmatites.
Uses & applications
Used as a flux in steel making, in the production of hydrofluoric acid, in high-performance telescopes and camera lenses, and widely collected as ornamental minerals or carved into jewelry and decorative items.
Geological facts
Fluorite is where the term 'fluorescence' comes from, as many specimens glow under ultraviolet light. It is often called 'the most colorful mineral in the world' because it occurs in every color of the rainbow.
Field identification & locations
Identify by its cubic crystal form and perfect cleavage that creates diamond-shaped fragments. It can be scratched by a steel knife but not by a copper penny. Found in famous localities like Illinois (USA), China, Mexico, and England.
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