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Kunzite
Known as the "evening" stone, Kunzite was discovered in 1902 and named
after G.F. Kunz - Tiffany's chief gemologist at the time and a noted mineralogist.
Kunzite is the pink variety of spodumene, which also includes a green
variety of gemstone known as Hiddenite. Kunzite is strongly pleochroic,
meaning there is a color intensity variation when a crystal is viewed
from the top or bottom than from other directions. The top and bottom
of the crystal reveal the deepest colors and knowledgeable gem cutters
take advantage of its effects. Kunzite's cellular structure gives it perfect
cleavage and so it is very sensitive to pressure along this cleavage plane.
Orientation of the gem material is critical to successful faceting of
this material. Due to Kunzite's cleavage, splintery fracture and strong
pleochroism it is considered a real gem cutters' challenge. However, its
lovely pink to violet color makes Kunzite an attractive and desirable
gemstone.
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The lithium in Kunzite's
chemical composition - LiAl (Si2O6), lithium aluminum silicate - gives
it a wonderful pink-violet color that compliments either fall or spring
wardrobes. It shows its color well in larger sizes. Since it is a pastel
gem, small sizes tend to be very pale. Kunzite needs a certain amount
of mass to bring out its color. Keep Kunzite out of direct sun or high
heat because it can fade. This fact has earned it the nickname: Evening
Stone. Jewelry featuring Kunzite should not be cleaned in an ultrasonic
or steam cleaner. Ionic cleaners and/or warm, soapy water and a soft brush
are the best ways to clean Kunzite.
Metaphysically, Kunzite gives off powerful love energy, promotes peace
and purification, dissipates negativity and is excellent for meditation.
The corresponding Astrological Signs for Kunzite are: Scorpio, Taurus,
& Leo.
Kunzite is mined in Afghanistan, Brazil, Burma, Canada, Madagascar, Malagasy
Republic, Mexico, Pakistan, Russia, Sweden and the United States. It is
a fragile stone with a hardness of 6-7. It is of a comparable value to
red Garnet.
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