
mineral
Green Fluorite (Botryoidal/Massive)
Calcium Fluoride (CaF2)
Hardness: 4 on Mohs scale; Color: Pale green to bluish-green; Luster: Vitreous to dull; Crystal structure: Isometric (though appearing massive/drusy here); Cleavage: Perfect octahedral; Specific gravity: 3.175-3.184.
- Hardness
- 4 on Mohs scale
- Color
- Pale green to bluish-green
- Luster
- Vitreous to dull
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Physical properties
Hardness: 4 on Mohs scale; Color: Pale green to bluish-green; Luster: Vitreous to dull; Crystal structure: Isometric (though appearing massive/drusy here); Cleavage: Perfect octahedral; Specific gravity: 3.175-3.184.
Formation & geological history
Formed through hydrothermal processes where hot fluorine-bearing fluids circulate through cracks in limestone or other rocks. This specific habit suggests lower temperature formation in cavities or veins.
Uses & applications
Used as a flux in steelmaking (fluorite), in the manufacture of glass and enamels, for carving decorative objects, and as a popular mineral specimen for collectors.
Geological facts
Fluorite is the origin of the term 'fluorescence' because many specimens glow under ultraviolet light. It is also the defining mineral for level 4 on the Mohs scale of mineral hardness.
Field identification & locations
Identified by its relatively low hardness (can be scratched by a knife but not a copper coin), its cubic cleavage fragments, and often its distinct colors. Commonly found in China, Mexico, and the UK (Durham).
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