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SYLVITE , a See also:mineral consisting of See also:potassium chloride (KCI), first observed in 1823, as an encrustation on Vesuvian See also:lava. Well-formed crystals were subsequently found in the See also:salt deposits of See also:Stassfurt in See also:Prussia and Kalusz in See also:Austrian See also:Galicia. It crystallizes in the cubic See also:system with the See also:form of 'cubes and cubooctahedra and possesses perfect cleavages parallel to the faces of the See also:cube. Although the crystals are very similar in See also:appearance to crystals of See also:common salt, they are proved by See also: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 See also:bright See also: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: SYLVITEAdditional information and CommentsThere are no comments yet for this article.
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