SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico)
SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico) SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico)

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SWJ0025 - Finest Grade Blue Fluorite Crystal Cluster from Blanchard Mine (New Mexico)

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Species
Fluorite
Age
-
Location
New Mexico, USA
Formation
Mining district: Blanchard Mine
Size
101 x 78 x 52 mm   •    in
Weight
650 g   •    oz
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Description

ORIGIN: New Mexico, USA
Mining district: Blanchard Mine

Size/Weight: 101 x 78 x 52mm - 605g

DESCRIPTION:
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon.

Fluorite is a colorful mineral, both in visible and ultraviolet light, and the stone has ornamental and lapidary uses. Industrially, fluorite is used as a flux for smelting, and in the production of certain glasses and enamels. The purest grades of fluorite are a source of fluoride for hydrofluoric acid manufacture, which is the intermediate source of most fluorine-containing fine chemicals. Optically clear transparent fluorite lenses have low dispersion, so lenses made from it exhibit less chromatic aberration, making them valuable in microscopes and telescopes. Fluorite optics are also usable in the far-ultraviolet and mid-infrared ranges, where conventional glasses are too absorbent for use.

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