Online Encyclopedia

SYLVITE

Online Encyclopedia
Originally appearing in Volume V26, Page 284 of the 1911 Encyclopedia Britannica.
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SYLVITE  , a

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mineral consisting of potassium chloride (KCI), first observed in 1823, as an encrustation on Vesuvian
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lava . Well-formed crystals were subsequently found in the salt deposits of
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Stassfurt in Prussia and Kalusz in
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Austrian Galicia . It crystallizes in the cubic
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system with the form of 'cubes and cubooctahedra and possesses perfect cleavages parallel to the faces of the cube . Although the crystals are very similar in appearance to crystals of
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common salt, they are proved by etching experiments to possess a different degree of symmetry, namely plagihedral-cubic, there being no planes of symmetry but the full number of axes of symmetry . Crystals are colourless (sometimes bright blue) and transparent; the hardness is 2 and the, specific gravity 1'93 . Like salt, it is highly diathermanous . The name sylvite or sylvine is from the old pharmaceutical name, sal digestivus sylvii, for this salt . (L . J .

End of Article: SYLVITE
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JOSHUA SYLVESTER (1563–1618)
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