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PEROVSKITE, or PEROFSKITE

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Originally appearing in Volume V21, Page 179 of the 1911 Encyclopedia Britannica.
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See also:

PEROVSKITE, or PEROFSKITE , a See also:mineral consisting of See also:calcium titanate, CaTiO3, usually with a small proportion of the calcium replaced by See also:iron. The crystals found in schistose rocks have the See also:form of cubes, which are sometimes modified on the edges and corners by numerous small planes; on the other See also:hand, the crystals occurring as an See also:accessory constituent of eruptive rocks are octahedral in form and microscopic in See also:size. Although geometrically cubic, the crystals 'are always doubly refracting, and they sometimes show See also:evidence of complex mimetic twinning; their structure as shown in polarized See also:light is very similar to that of the mineral See also:boracite, and they are therefore described as pseudo-cubic. There are distinct cleavages parallel to the faces of the See also:cube. The See also:colour varies from See also:pale yellow to blackish-See also:brown and the lustre is adamantine to metallic; the crystals are transparent to opaque. The See also:index of See also:refraction is high, the hardness 5z and the specific gravity 4.0. The mineral was discovered at Achmatovsk near Zlatonst in the Urals by G. See also:Rose in 1839, and named in See also:honour of See also:Count L. A. Perovsky;at this locality large cubes occur with See also:calcite and See also:magnetite in a See also:chlorite-schist. Similar crystals are also found in See also:talc-schist at See also:Zermatt in See also:Switzerland. The microscopic octahedral crystals are characteristic of melilite See also:basalt and See also:nepheline basalt; they have also been found in See also:peridotite and See also:serpentine.

(L. J.

End of Article: PEROVSKITE, or PEROFSKITE

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