
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: typically green, purple, yellow, or blue; Luster: vitreous (glassy); Crystal structure: isometric/cubic; Cleavage: perfect octahedral; Specific gravity: 3.18
- Hardness
- 4 on Mohs scale
- Color
- typically green, purple, yellow, or blue
- Luster
- vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale; Color: typically green, purple, yellow, or blue; Luster: vitreous (glassy); Crystal structure: isometric/cubic; Cleavage: perfect octahedral; Specific gravity: 3.18
Formation & geological history
Usually forms in hydrothermal veins, often associated with metallic ores. It can be found in sedimentary environments or as an accessary mineral in igneous rocks like granites.
Uses & applications
Used in the manufacture of steel, glass, and hydrofluoric acid. High-clarity specimens are used for specialized optical lenses. Tumbled stones are used in jewelry and crystal collecting.
Geological facts
Fluorite is the origin of the term 'fluorescence' because many specimens glow under ultraviolet light. It is often called 'the most colorful mineral in the world'.
Field identification & locations
Identify in the field by its distinct cubic crystal habit, perfect cleavage into octahedrons, and the fact that it can be scratched by a steel knife but not a copper penny. Common locations include China, Mexico, and Illinois, USA.
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