Online Encyclopedia

HYACINTH, or JACINTH

Online Encyclopedia
Originally appearing in Volume V14, Page 25 of the 1911 Encyclopedia Britannica.
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HYACINTH, or JACINTH  , in
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mineralogy, a variety of
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zircon (q.v.) of yellowish red colour, used as a gem-stone . The
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hyacinthus of ancient writers must have been our
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sapphire, or blue
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corundum, while the hyacinth of
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modern mineralogists may have been the stone known as lyncurium (AuyKOU;iiov) . The
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Hebrew word leshem, translated ligure in the Authorized Version (Ex.
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xxviii . 19), from the X yuprov of the Septuagint, appears in the Revised Version as jacinth, but with a marginal alternative of
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amber . Both jacinth and amber may be reddish yellow, but their identification is doubtful . As our jacinth (zircon) is not known in ancient
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Egyptian
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work, Professor Flinders Petrie has suggested that the leshem may have been a yellow
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quartz, or perhaps
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agate . Some old
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English writers describe the jacinth as yellow, whilst others refer to it as a blue stone, and the hyacinthus of some authorities seems undoubtedly to have been our sapphire . In Rev. xx . 20 the Revised Version retains the word jacinth, but gives sapphire as an alternative . Most of the gems known in trade as hyacinth are only garnets—generally the deep orange-brown hessonite or
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cinnamon-stoneand many of the antique engraved stones reputed to be hyacinth are probably garnets . The difference may be detected optically, since the garnet is singly and the hyacinth doubly refracting; moreover the specific gravity affords a
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simple means of diagnosis, that of garnet being only about 3.7, whilst hyacinth may have a density as high as 4.7 . Again, it was shown many years ago. by
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Sir A .

H .

Church that most hyacinths, when examined by the spectroscope, show a series of dark absorption bands, due perhaps to the presence of some rare element such as uranium or erbium . Hyacinth is not a
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common
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mineral . It occurs, with other zircons, in the gem-gravels of
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Ceylon, and very
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fine stones have been found as pebbles at Mudgee in New South Wales . Crystals of zircon, with all the typical characters of hyacinth, occur at Expailly, Le
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Puy-en-Velay, in Central France, but they are not large enough for cutting . The stones which have been called Compostella hyacinths are simply ferruginous quartz from Santiago de Compostella in Spain . (F . W .

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