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VESUVIANITE , a See also:rock-forming See also:mineral of complex com-
position. It is a basic See also:calcium and See also:aluminium silicate See also:con-
aining small amounts of See also:iron, See also:magnesium, See also:water,
See also:fluorine, etc., and sometimes See also:boron; the ap-
proximate See also:formula is H2Ca6(Al,Fe)aSi5O18. It
crystallizes in the tetragonal See also:system, but often
exhibits See also:optical anomalies, and the optical sign
varies from See also:positive to negative. Well-devel-
oped crystals are of frequent occurrence. They
usually have the See also:form of four- or eight-sided
prisms terminated by the basal planes (c) and
See also:pyramid-planes (p in fig.); the See also:prism-planes are vertically
striated and the basal planes smooth and See also:bright. Crystals are
transparent to translucent, vitreous in lustre and vary in See also:colour from See also: See also:Hauy (1796), is now in See also:common use.
Vesuvianite is typically a mineral of contact-metamorphic origin, occurring most frequently in crystalline limestones at their contact with igneous rock-masses; it also occurs in See also:serpentine, See also:chlorite-schist and See also:gneiss, and is usually associated with See also:garnet, See also:diopside, See also:wollastonite, &c. Localities which have yielded fine crystallized specimens are the See also:Ala valley near See also:Turin, See also:Piedmont, Monte Somma (Vesuvius), Monzoni in the Fassa valley, See also:Tirol, Achmatovsk near Zlatonst in the Urals, the See also:River Wilui See also:district near See also:Lake See also:Baikal in See also:Siberia (" wiluite "), See also:Christiansand in See also:Norway, &c. When found in transparent crystals of a See also:good green or brown colour it is occasionally cut as a See also:gem-See also: Additional information and CommentsThere are no comments yet for this article.
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