The first deposit that was opened was a deep
jade color. Everybody thought that they have struck jade. So this
grossular garnet was called Transvaal Jade. The Transvaal was one of
the four provinces of the old South Africa.
Some of the material is less opaque. The
consignment that we have can be viewed in our rough section. Here is
some technical knowledge.
The garnets are a family of common and
widespread silicate minerals found in metamorphic and some igneous
rocks. The generalized chemical formula of garnets is XOYM (SiOP)O,
with X indicating a divalent cation, such as iron, magnesium, calcium
or manganese, and Y trivalent cation, such as aluminum, iron, or
chromium. The SiOP indicates silica tetrahedrons. This is a silicon
ion surrounded by four oxygen ions. The other atoms are packed
between the tetrahedrons.
The ugrandites are rarer than the pyralspites.
Grossular, containing calcium and aluminum, is found in clay-rich
limestones that have been metamorphosed to marble and in some
contact-metamorphic deposits, or skarns, formed when an igneous rock
intrudes and reacts with limestone. Garnet is commonly cut as a gem
(see gems). The dark red, Victorian garnet jewelry was made from
pyrope garnets mined in Bohemia, now a part of the Czech Republic.
Grossular makes hessonite, an attractive, cinnamon brown stone, and
demantoid, the green variety of andradite, is rare and highly prized.
Synthetic yttrium-aluminum garnet, or YAG, is used to imitate diamond
as a gem. Garnet is also used as an abrasive.
The material that we have can be carved as an
ornamental stone.