Fluorite (also called
fluor-spar or
Blue John) is a
mineral composed of
calcium fluoride, CaF
2. It is an isometric mineral with a cubic habit, though octohedrons and dodecahedrons are not uncommon.
Occurrence
Fluorite may occur as a vein deposit, especially with metallic minerals, where it often forms a part of the gangue (the worthless `host-rock' in which valuable minerals occur) and may be associated with
barite,
quartz and
calcite. It is a common mineral in deposits of
pneumatolytic[?] origin and has been noted as a primary mineral in
granites and other
igneous rocks.
One of the most famous of the older localities of fluorite is
Derbyshire,
England, where under the name of Derbyshire
Blue John beautiful blue fluorite is used for ornamental purposes; its softness, however, has been a bar to general use.
Uses
As well as ornamental uses, fluorite is also used as a flux in the manufacture of steel, in the making of opalescent[?] glass, enamels[?] for cooking utensils, and for hydrofluoric acid[?]. The name fluorite is derived from the Latin fluo, flow, in reference to its use as a flux.
Details
*Note on colours:
The blue kind is often a delicate violet-blue, sometimes
amethystine in tint. Certain specimens appear blue by reflected light and green or yellow by transmitted light. Fluorite sometimes
phosphoresces[?] when heated or scratched. Other varieties
fluoresce beautifully under the influence of
X-rays or
ultraviolet light.
See also: List of minerals
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