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SAPPHIRE

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Originally appearing in Volume V24, Page 202 of the 1911 Encyclopedia Britannica.
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SAPPHIRE ,1 a See also:

blue transparent variety of See also:corundum, or native alumina, much valued as a See also:gem-See also:stone. It is essentially the same See also:mineral as See also:ruby, from which it differs chiefly in See also:colour. The colour of the normal sapphire varies from the palest blue to deep See also:indigo, the most esteemed tint being that of the blue cornflower. Many of the crystals are parti-coloured, the blue being distributed in patches in a colourless or yellow stone; but by skilful cutting, the deep-coloured portion may be caused to impart colour to the entire gem. As the sapphire crystallizes in the hexagonal See also:system it is dichroic, but in See also:pale stones this See also:character may not be well marked. In a deep-coloured stone the colour may be resolved, by the dichroscope, into an See also:ultramarine 1 Indirectly from Gr. o&orq5uupos, but there seems no doubt that this See also:term, like the See also:Hebrew sapir of the Old Testament, was formerly applied to what is now called lapis lazuli; the See also:modern sapphire was probably known as u&xwOos (See also:hyacinthus). colour. It is a silicate, containing See also:aluminium, See also:magnesium and See also:iron, brought originally from See also:Greenland, and since found in a See also:rock from the See also:Vizagapatam See also:district in See also:India. (F. W.

End of Article: SAPPHIRE

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SAPPHIC METRE, SAPPHICS
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SAPPHO (7th–6th centuries B.C.)