
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 (Mohs scale); Color: Purple, green, yellow, or clear; Luster: Vitreous; Crystal structure: Isometric (often cubic or octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.175-3.184
- Hardness
- 4 (Mohs scale)
- Color
- Purple, green, yellow, or clear
- Luster
- Vitreous
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Physical properties
Hardness: 4 (Mohs scale); Color: Purple, green, yellow, or clear; Luster: Vitreous; Crystal structure: Isometric (often cubic or octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.175-3.184
Formation & geological history
Predominantly formed in hydrothermal veins, often associated with metallic ores like lead and silver. It can also occur in sedentary environments or as an accessory mineral in igneous rocks.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, in high-performance telescopes and camera lenses, and widely in jewelry and mineral collecting.
Geological facts
Fluorite gave the name to the phenomenon of fluorescence in 1852. It is often called 'the most colorful mineral in the world' because of its wide range of brilliant colors.
Field identification & locations
Identified in the field by its distinct 4-directional cleavage and its inability to scratch glass but being easy to scratch with a knife. Common locations include China, Mexico, South Africa, and Illinois in the USA.
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