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CHRYSOPRASE (Gr. Xpvvor, gold, and ap...

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Originally appearing in Volume V06, Page 321 of the 1911 Encyclopedia Britannica.
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CHRYSOPRASE (Gr. Xpvvor, gold, and apaorov,
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leek)
  , a name applied by
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modern mineralogists to an apple-green variety of chalcedony or hornstone, used as an ornamental stone . The colour is due to the presence of nickel, probably in the form of a hydrous silicate . By exposure to a moderate heat, or to strong
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light, the chrysoprase becomes paler, or even colourless, but it may regain its colour by absorption of moisture . Chrysoprase is a
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mineral of rather limited distribution . Most of it comes from the neighbourhood of
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Frankenstein in
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Silesia, where it occurs in association with altered
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serpentine . It is found to a limited extent at Revdinsk, near
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Ekaterinburg, in the Urals; and it occurs also in India . It is known, too, at several localities in North
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America, notably at Nickel Mount, Douglas county,
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Oregon, where it occurs in nickeliferous serpentine . The chrysoprase of the moderns is certainly not the chrysoprasius of Pliny, or the Xpvalnrpaaos of Greek writers . The ancient stone was not improbably our
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chrysoberyl, and it is doubtful whether the modern chrysoprase was known until a comparatively
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late period . The chrysoprase of Kosemutz, near Frankenstein in Silesia, was discovered in 1740, and used by Frederick the
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Great in the decoration of the palace of Sans Souci at
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Potsdam . But at a much earlier date the Silesian chrysoprase was used for mural decoration at the Wenzel
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chapel at Prague . Chrysoprase was a favourite stone in England at the beginning of the 19th century, being set round with small brilliants and used for brooches and rings .

At the

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present time it is said to be regarded by some as a " lucky stone." Much commercial chrysoprase is chalcedony artificially stained by impregnation with a green salt of nickel . (F . W .

End of Article: CHRYSOPRASE (Gr. Xpvvor, gold, and apaorov, leek)
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