Online Encyclopedia

ALEXANDRITE

Online Encyclopedia
Originally appearing in Volume V01, Page 576 of the 1911 Encyclopedia Britannica.
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ALEXANDRITE  , a variety of

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chrysoberyl (q.v.) discovered in the Urals in 1833, on the day set apart for celebrating the majority of the
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cesarevich, afterwards the
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tsar, Alexander II., in whose honour the stone was named by Nils Gustaf Nordenskiold, of Helsingfors . It is remarkable for being strongly dichroic, generally appearing dark green by daylight and
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raspberry-red by candle-
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light, or by daylight transmitted through the stone . As red and green are the military colours of Russia, the
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mineral became highly popular as a gem-stone . The dark green crystals are usually cloudy and cracked, and grouped in triplets presenting a pseudo-hexagonal form . Alexandrite was found originally in the
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emerald- mine of Takovaya, east of
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Ekaterinburg in the Urals, and afterwards in the gold-bearing sands of the Sanarka in the
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southern Urals . Subsequently it was discovered in greater abundance in the gem-gravels of
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Ceylon . It has been found also in
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Tasmania . Some of the Ceylon alexandrite exhibits, when suitably cut, the Cat's-eye chatoyance, whence it has been called alexandrite cat's-eye . (F . W .

End of Article: ALEXANDRITE
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