Topaz (To-Paz):
The roots of the word Topaz
first burgeoned into life in ancient Egypt, circa 300B.C.,
under the Pharaoh Ptolemy II. However, what the Egyptians,
Greeks and subsequent Romans came to refer to as Topaz
was in fact our peridot: In reality the mineral that
we call Topaz
today, has only been officially recognized since the
17th Century. Initially, hundreds of kilos of Topaz were sourced
from Saxony in East Germany, later massive deposits
were also found in South America.
Topaz
was first discovered in the 'New World', under the reigning
Portuguese colonialists, in the Brazilian mines of Villa
Rica, near Ouro Preto. From these mines came a colored
Topaz
never seen before. Owing to the Portuguese royal family's
love of these gems,
this variety received one of Topaz's most prestigious
titles.
'Imperial Topaz' is the most coveted of all the Topaz
family. Its name is used to denote colors that fall
between a scintillating golden orange and pink nuance. Of all Imperial Topaz's hues the most highly prized is the pink
variety. For the most part these Pink Topazes are sourced
from the mines of Ouro Preto in Brazil, and the Katlang
region in Pakistan. Most Pink Topaz
derives its color from chromium present within the gems
crystal structure. Heating the dark-yellow variety of
Topaz
can also produce pink Topaz.
Naturally occurring Yellow and Brown Topaz
owe their colors to 'Color Centers,' the infamous 'Swiss,'
'Sky' and 'London' Blue Topaz
are often derived from these two sources by irradiating
the Yellow and Brown 'Color Centers.'
Color centers are the cause of color within Blue Topaz
crystals; they result from defects within the atomic
structure of the crystal, which cause certain colors
to become visible by the absorption of other light waves.
Color centers are formed due to exposure to gamma rays;
this irradiation may be from both natural and artificial
sources. When exposed to radioactive sources, both natural
and artificial, electrons within the atomic structure
of Topaz
can be removed from their normal sites. Some electrons
are bounced around, eventually coming to rest in a vacant
part of the atomic structure called a trap. Electrons
in specific traps absorb a certain range of light wavelengths,
the visible color that you see is the color that is
not absorbed by these trapped electrons.
Naturally occurring 'Colorless,' or 'White,' Topaz
takes a very high polish and is wonderfully clear and
transparent. A relative new comer to the Topaz
family is Mystic Topaz,
which is produced by taking 'Colorless' Topaz
and applying a thin layer of titanium oxide via physical
vapor deposition. This process is similar to the method
used in coating camera lenses, and produces an iridescent
effect across the gems
surface. Mystic Topaz,
coming in a wide variety of colored nuances, is extremely
popular and one of the most successful colored gemstones
available today.
Topaz
crystallizes from fluorine-bearing vapor in last stages
of solidification of igneous rocks. In mineralogical
terms it is a silicate of aluminium and fluorine denoted
by the chemical formula Al2SiO4(F,OH)2. It is found
in association with granite rocks, within pegmatite
veins, and in secondary concentrations such as streambed
alluvial deposits.
Topaz
crystals form in the rhombic system of crystallization,
and its crystals are prismatic. Topaz
possesses a perfect basal cleavage; therefore gems
should be handled with care. Despite this fact, Topaz
is one of the hardest minerals known to man attaining
an 8 out of 10 on the Moh's hardness scale, second only
to corundum and diamond. Most Topaz
is transparent to translucent with a vitreous glass-like
luster. However, naturally occurring Pink and Red Topaz
is often included due to the presence of the impurity
chromium. These pink colored Topazes are so rare that
the inclusions are, much like with ruby, tolerated and
even valued as identifying fingerprints.
Topaz
is sourced from the mines of Ouro Preto and Minas Gerais
in Brazil, the Ural and Ilmen Mountains in Russia, Pakistan,
Sri Lanka, Czech Republic, Saxony, Norway, Sweden, Japan,
Mexico and the United States.