
mineral
Fluorite (Blue)
Calcium Fluoride (CaF2)
AI-generated identification · may be incorrectHardness: 4 on Mohs scale. Color: Deep blue to teal with internal inclusions. Luster: Vitreous (glassy). Crystal structure: Cubic (though this is tumbled/rounded). Cleavage: Perfect octahedral. Specific gravity: 3.175–3.184.
- Hardness
- 4 on Mohs scale
- Color
- Deep blue to teal with internal inclusions
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 4 on Mohs scale. Color: Deep blue to teal with internal inclusions. Luster: Vitreous (glassy). Crystal structure: Cubic (though this is tumbled/rounded). Cleavage: Perfect octahedral. Specific gravity: 3.175–3.184.
Formation & geological history
Formed through hydrothermal activity, often as a vein mineral in igneous rocks or as a precipitate in sedimentary settings. It occurs in a variety of geological ages from Paleozoic to more recent formations depending on local tectonic activity.
Uses & applications
Used as a flux in steel making, in the manufacture of hydrofluoric acid, and for high-performance telescoping and camera lenses. In its gemstone form, it is used for jewelry, lapidary art, and metaphysical collecting.
Geological facts
Fluorite is the mineral from which the term 'fluorescence' was derived, as many specimens glow under UV light. It is often called 'the most colorful mineral in the world' because it can occur in every color of the spectrum.
Field identification & locations
Identify in the field by its distinct cubic crystal habit (if not tumbled) and limited hardness; it can be scratched by a steel knife but not by a copper penny. Commonly found in China, Mexico, South Africa, and the Illinois-Kentucky Fluorspar District. Look for vitreous luster and distinct color zoning.
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