
mineral
Fluorite
Calcium fluoride (CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale; Color: Purple, green, clear, or multi-colored; Luster: Vitreous; Crystal system: Isometric/Cubic; Cleavage: Perfect octahedral; Specific gravity: 3.175–3.184
- Hardness
- 4 on Mohs scale
- Color
- Purple, green, clear, or multi-colored
- Luster
- Vitreous
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Physical properties
Hardness: 4 on Mohs scale; Color: Purple, green, clear, or multi-colored; Luster: Vitreous; Crystal system: Isometric/Cubic; Cleavage: Perfect octahedral; Specific gravity: 3.175–3.184
Formation & geological history
Formed through hydrothermal activity, typically occurring as a vein mineral in carbonate rocks or as a primary mineral in granites and other igneous rocks. Formed across various geological ages.
Uses & applications
Used as a flux in steelmaking/smelting, in glass making, for manufacturing hydrofluoric acid, and as a semi-precious gemstone for jewelry and ornamental carvings.
Geological facts
Fluorite is often strongly fluorescent under UV light. It is known as the 'most colorful mineral in the world' due to the wide range of hues caused by impurities.
Field identification & locations
Identified by its four directions of perfect cleavage (forming octahedrons), its hardness (softer than glass), and its distinctive range of colors. Common in China, Mexico, South Africa, and the USA (Illinois/Kentucky).
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous