Gemstone GlossaryRhodolite Garnet The history of Garnet dates back to the Bronze Age (more than 5,000 years ago), when it was a very popular gemstone. According to Christian and Jewish mythologies, when God's wrath clouded the earth with thunderous storms and endless rain during the Great Flood, a radiant red Garnet guided the way for Noah, ultimately leading his ark to salvation. Unlike other gemstones, Garnets are believed to contain both protective and
destructive elements. The Crusaders set Garnets into their body armor, believing
the protective power of the stones would lead them to safety. Conversely, some
Asian cultures added Garnets to bullets, believing its destructive power would
greatly amplify the enormity of a wound. Garnets are found in a wide variety of locations including: Kenya, Sri Lanka, Thailand, Brazil, India & Arizona (USA), however the bulk of today's Garnet supplies come from Africa. When evaluating Garnets, color is the most important characteristic. The color must be intense and uniform with a tone that is not too light or too dark. Fine Garnets should be eye clean with minimal inclusions under magnification. Size is also a very critical determinant of the stone's value. Garnets are a group of related minerals, containing cubic crystalline structure with slight variations in their chemical compositions. In all, there are 7 major types of Garnets, which include Almandine, Pyrope, Spessartine, Grossular, Andradite, Rhodolite and Malaia. Many consider Rhodolite to be the "Queen of Garnets", due to its
delicate pink to violet red color, reminiscent of the rhododendron flower (a
common symbol of feminine beauty). Chemically, this Garnet's composition is
a blend of Almandine and Pyrope. The most spectacular pink Rhodolites are mined
in Sri Lanka, Tanzania and Zimbabwe.
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