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The mineral topaz is a nesosilicate of aluminum and fluorine with
the chemical formula Al2SiO4(F,OH)2. It crystallizes in the
orthorhombic system and its crystals are mostly prismatic terminated
by pyramidal and other faces, the basal pinacoid often being
present. It has an easy and perfect basal cleavage and so gemstones
or other fine specimens should be handled with care to avoid
developing cleavage flaws. The fracture is conchoidal to uneven.
Topaz has a hardness of 8, a specific gravity of 3.4-3.6, and a
vitreous lustre. Pure topaz is transparent but is usually tinted by
impurities; typical topaz is wine or straw-yellow. They may also be
white, gray, green, blue, or reddish-yellow and transparent or
translucent. When heated, yellow topaz often becomes reddish-pink.
It can also be irradiated, turning the stone a light and distinctive
shade of blue. A recent trend in jewelry is the manufacture of topaz
specimens that display iridescent colors, by applying a thin layer
of titanium oxide via physical vapor deposition. |
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Topaz is found associated with the more acid rocks of the granite
and rhyolite type and may be found with fluorite and cassiterite. It
can be found in the Ural and Ilmen mountains, Czech Republic,
Saxony, Norway, Sweden, Japan, Brazil, Mexico, and the United States
The name "topaz" is derived from the Greek topazos, "to seek," which
was the name of an island in the Red Sea that was difficult to find
and from which a yellow stone (now believed to be a yellowish
olivine) was mined in ancient times. In the Middle Ages the name
topaz was used to refer to any yellow gemstone, but now the name is
only properly applied to the silicate described above.
According to Rebbenu Bachya, the word "Leshem" in the verse Exodus
28:19 means "Topaz" and was the stone on the Ephod representing the
tribe of Dan.
Topaz is also the birthstone of November.
The silicate minerals make up the largest and most important class
of rock-forming minerals. They are classified based on the structure
of their silicate anion group.
A crystal is a solid in which the constituent atoms, molecules, or
ions are packed in a regularly ordered, repeating pattern extending
in all three spatial dimensions.
Generally, crystals form when they undergo a process of
solidification. Under ideal conditions, the result may be a single
crystal, where all of the atoms in the solid fit into the same
crystal lattice or crystal structure but, generally, many crystals
form simultaneously during solidification, leading to a
polycrystalline solid. For example, most metals encountered in
everyday life are polycrystals. Crystals are often symmetrically
intergrown to form crystal twins.
Which crystal structure the fluid will form depends on the chemistry
of the fluid, the conditions under which it is being solidified, and
also on the ambient pressure. The process of forming a crystalline
structure is often referred to as crystallization.
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