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Rhodolite
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.
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The name "Garnet" is believed to have derived
from "pomegranate" with its red, "Garnet colored" seeds. While the name
Garnet has long been associated with a rich red color, the gemstone actually
comes in a much wider array of color variations including: reds, oranges,
greens and color change.
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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