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Garnet

Garnet is not a single mineral, but rather a group of similar minerals known as the "garnet group." All the natural garnets are complex silicates that differ in chemical composition, but have almost identical atomic structures. Garnets are not only red; they may be orange, yellow, brown, pale green, deep green, violet, purple, or even colorless.

 

Garnet is a truly ancient gem, known thousands of years before the birth of Christ. In those early days of civilization garnet, along with other gems, was known as "carbuncle." Although this term was generally applied to any red gem, today only red cabochon-cut garnets are called carbuncles.
 

As with most other stones, garnets were considered to have great curative powers, especially against fevers. The wearer of a garnet was supposed to be protected in his travels and kept in good health. The name "garnet" comes from the Latin word "granatus," meaning "like seeds," because garnets in a rock look somewhat like the seeds in a pomegranate.

Garnet

The Victorian era made extensive use of reddish garnets mined in Bohemia (now Czechoslovakia). These became quite popular and were widely used in low-cost jewelry, thus popularizing garnet as a gem and,Unfortunately, cheapening its image. Reddish-brown garnets are still very inexpensive, although red, violet, and purple gems can be fairly costly, especially in larger sizes.


Garnet, with its large range of colors, is perhaps the most underrated all gems. Nearly all the garnet species have gem potential. They are all about the same hardness, 6'/z-7'/s on the Mohs scale, and none show cleavage, thus making them suitable for any type of jewelry. Cut garnets an be very brilliant and show rich, lovely colors that look good both in light and in artificial light.

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There are basically six major garnet species:Pyrope is usually blood-red in color, sometimes with a tinge of purple or -brown. Finer grades may resemble ruby. Most pyropes have some inclusions, and fine gem material is scarce, especially rough that will provide large cut gems. Such material is known from only a few localities. The U.S.S.R. is a source of magnificent gemstones.

Good pyrope is associated with the diamond in South African kimberlite otpes. Brazil and Australia have produced good stones, and pyrope has been found in the United States in Arizona, Colorado, and New Mexico. Almandine today satisfies world demand for an inexpensive red gem¬-- me. Almandine is the most common garnet seen in jewelry. Its ,colorranges from dark red to brownish-red.

The finer grades are almost indistinguishable at sight from pyrope. Good gem material comes from Sri Lanka, India, Brazil, Alaska, and Africa.

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