Fluorite,
calcium fluoride is a major industrial mineral used as a flux in
steel making as well as in the preparation of hydrofluoric acid and
in the ceramics industry. Mainly used for glasses and enamels.
Fluorite's
vitreous, cubic crystals (isometric system)
and cleavable, granular masses have a wide color range (often green,
blue, or purple) and may fluoresce under ultraviolet light. Hardness
is 4, specific gravity 3.0-3.3. Fluorite deposits form under a wide
variety of conditions: as veins produced by hydrothermal alteration,
as beds and cavities in sedimentary rocks, in hot spring deposits,
and in pegmatites.
It forms the typical cube and to a lesser
extent, the octahedron as well as combinations of these two and other
rarer isometric habits. Always with equate crystals; less common are
crusts and botryoidal forms. Twinning also produces penetration twins
that look like two cubes grown together.
Cleavage is perfect in 4 directions forming octahedrons.
Sometimes the less common habits such as a
colored octahedron are seen inside of a colorless cube. One crystal of Fluorite
could potentially have four or five different color zones or bands.
Fluorite
is frequently fluorescent and, like its normal light colors, its
fluorescent colors are extremely variable. Typically it fluoresces
blue but other fluorescent colors include yellow, green, red, white
and purple. The word fluorescent was derived from fluorite since
specimens of Fluorite
were some of the first fluorescent specimens ever studied.
The naming followed the naming precedence set
by opalescence from opal;
ergo fluorescence
from Fluorite.
Another unique luminescent property of
fluorite is its thermoluminescence. Thermoluminescence
is the ability to glow when heated. Not all fluorites do this, in
fact it is quite a rare phenomenon. A variety of fluorite known as "chlorophane"
can demonstrate this property very well and will even thermoluminesce
while the specimen is held in a person's hand activated by the
person's own body heat (of course in a dark room, as it is not bright
enough to be seen in daylight). The thermoluminescence is green to
blue-green and can be produced on the coils of a heater or electric
stove top. Once seen, the glow will fade away and can no longer by
seen in the same specimen again. It is a one shot deal.
Fluorite has other qualities besides its great
color assortments that make it a popular mineral. It has several
different crystal habits that always produce well formed, good, clean
crystals. The cube is by far the most recognized habit of fluorite
followed by the octahedron which is believed to form at higher
temperatures than the cube. Although the cleavage of fluorite can
produce an octahedral shape and these cleaved octahedrons are popular
in rock shops the world over, the natural (e.g. uncleaved)
octahedrons are harder to find.
Fluorite, as mention above, has octahedral
cleavage. This means that it has four identical directions of
cleavage and when cleaved in the right ways can produce a perfect
octahedral shape. Many thousands of octahedrons are produced from
massive or large undesirable crystals of fluorite (hopefully!) and
are sold in rock shops and museum gift shops at a small cost.
Fluorite mine workers are reported to sit down at lunch breaks and
cleave the octahedrons for the extra cash. The octahedrons are very
popular due to their attractive colors, clarity,
"diamond-shaped" and low costs, but to a serious collector
they are nothing more than "cleavage fragments".
Fluorite not only is attractive in its own
right but is often associated with other attractive minerals.
Fluorite crystals will frequently accompany specimens of silver gray
galena, brassy yellow pyrite, chalcopyrite or marcasite, golden
barite, black sparkling sphalerite, intricately crystallized calcite
and crystal clear quartz, even amethyst.
The origin of the word fluorite comes from the
use of fluorite as a flux in steel and aluminum processing. It was
originally referred to as fluorospar by miners and is still called
that today.Fluorite is the most popular mineral for mineral
collectors in the world, second only to quartz. Every mineral
collection owned by even the newest and youngest of mineral
collectors must have a specimen of fluorite. Fluorite is by far one
of the most beautiful and interesting minerals available on the
mineral markets