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SYLVITE , a See also: mineral consisting of 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 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 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 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
.
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