
mineral
Fluorite
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: Yellow (in this specimen), can be purple, green, or blue; Luster: Vitreous; Crystal system: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.18
- Hardness
- 4 on Mohs scale
- Color
- Yellow (in this specimen), can be purple, green, or blue
- Luster
- Vitreous
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Physical properties
Hardness: 4 on Mohs scale; Color: Yellow (in this specimen), can be purple, green, or blue; Luster: Vitreous; Crystal system: Isometric (cubic/octahedral); Cleavage: Perfect octahedral; Specific gravity: 3.18
Formation & geological history
Formed in hydrothermal veins, often associated with metallic ores like lead and silver. It can also occur in sedimentary rocks such as limestone or in some igneous rocks like granite pegmatites.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, in high-performance telescopes and camera lenses, and widely as a decorative gemstone or mineral specimen.
Geological facts
Fluorite was the first mineral for which the phenomenon of fluorescence was named, as many specimens glow under ultraviolet light. It is also known as 'the most colorful mineral in the world'.
Field identification & locations
Identified in the field by its octahedral cleavage (it can be broken into 8-sided shapes), its relatively low hardness (can be scratched by a knife), and its vitreous luster. Commonly found in China, Mexico, and the USA (Illinois/Kentucky).
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Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
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Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
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Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic