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Yellow-blue
s pecimen - Yellow vein - Valzergues fluorite mine
Collection Gilles Emringer.
HISTORY
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Fluorite
is the most important natural fluoride. It can be found in many
veins that are often
associated to granitic rocks. Due to its richness and its colors,
the fluorite has always been fascinating for the man. This mineral
received several names (Spatum vitreum, Calx fluorata...) before
being called fluorite. The commercial and industrial word is fluorspar
(spathfluor in French...)
Its
crystallographic structure, very simple, was determined by William
H. Bragg. This was done by x-rays diffraction.
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Blue Fluorite - Cave-in-Rock - USA
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Fluorite
octahedrons on calcite
Mont-Blanc
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Cluster
of yellow fluorite cubes, disposed like a stalactite
Valzergues - Yellow Vein
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GENERAL INFORMATION :
Chemical
class : HALIDES
Crystalline system : CUBIC
Etymology : from Latin « fluere »= to flow - use in metallurgy.
Morphology : cubical, octahedral...
Color : from colorless to all colors.
Hardness : 4 (Mohs scale)
Index of refraction : n
= 1.434
Average density = 3.13
Melting point : 1360 °C
Transparency : all optical qualities are found (from
gem to stone).
Fluorescence : UV (long and short waves).
Solubility : in various acids, and aqueous solutions.
Pseudomorphosis : often
quartz.
Use : mainly in metallurgy and chemical industries.
Gitology : formation at low temperature. Especially often found in France.
Fluorite deposits:
-in the form of the principal mineral (see page "Mines
of fluorite")
-in the form of a secondary mineral (see page "Other
mines")
Valzergues
mine is a typical exemple of hydrothermal
veins.
A
nice specimen from the Yellow Vein (two sides).The color is very interesting
(honey-amber)
HABITUS
The
major part of crystallisations is cubic. Parallelepipedic crystals are
less often found.
Octahedral shapes appear when the temperature in which crystallisation
can occur is higher.
At last, the fluorite can be in the form of spheres like crystallisations
coming from Mahodarry (India)…
Many
intermediate shapes can also exist.(hexaoctahedron, tetra hexahedron…etc).
The
size of the crystals can reach impressive dimensions and weight
(A 100 kg single crystal was collected in the Valzergues mine - see
book page 157)
Twins
can also be found (« Cumberland » twins). Epitaxies and pseudomorphosis
appear in some mines.
COLOURING

El
Hammam - Morocco
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Berbes
- Spain
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Mina
Emilio - Spain
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Caravia
- Spain
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Argbla
- Morocco
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Argbla
- Morocco
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China
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Spain
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The
colouring is due to the presence of various compounds in the crystal :they
can be ions (yttrium, europium…).
The
most widespread colors are :
-
violet, light purple to dark purple (Berbès …)
- blue (Beix, Burg…)
- pink (Mont-Blanc…)
- yellow (Valzergues)
- green (La Barre…)
Crystallisations can also have an association of colors (for instance
: Valzergues
where yellow fluorites have a blue-purple edging).
Heating
and light tend to make
the colour of the crystals disappear.
Consequently, it is recommended to store the samples in darkness.
The
notoriety of Valzergues fluorite comes from the rarety of its color.
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Amber, purple and deep yellow with blue edge...
Specimens from the "yellow vein" - Valzergues - Aveyron
- France
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The
Rogerley fluorite is world-known for its dichroism.
Left : artificial lighting
Right : Natural ligh
Photos Jesse Fischer - private coll..
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INDUSTRY
The
use of fluorite as an industrial mineral is recent. Until the half of
the XIX century, its interest was mainly ornamental. Then, it became industrial
in the 1980s. The industrial growth goes back to 1860-1880. Currently,
the fluorite is mainly used in the following fields:
Chemical
industries (manufacturing of hydrofluoric acid, thermic fluids…)
Iron and steel industries (melting in the blast furnaces…)
…and
in fields of less economic importance.
Industries
of glass and ceramics
Welding…
Valzergues
fluorite was primaly used in iron and steel industries, in various factories
located anywhere in France. It was exported to the United States, too.
Fluorite
pictures on spathfluorminerals.com

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