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PYROXENE

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Originally appearing in Volume V22, Page 696 of the 1911 Encyclopedia Britannica.
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PYROXENE , an important See also:

group of See also:rock-forming minerals, very similar in chemical See also:composition and See also:general characters to the amphiboles (q.v.). Although crystallizing in three different systems, they all possess distinct prismatic cleavages, the angles between which are about 87° (the cleavage See also:angle in the amphiboles being 56°). They are metasilicates, but, as shown in the following table, the composition varies widely in the different See also:species, with corresponding See also:differences in the various See also:physical characters. The name pyroxene was originally given by R. J. Haiiy in 1796 to the See also:black crystals of See also:augite found in the lavas of See also:Vesuvius and See also:Etna: he derived the name from the See also:Greek a6p (See also:fire) and ivos (a stranger), because he thought that the crystals had been accidentally caught up by the lavas which contained them. As a See also:matter of fact, the pyroxenes are, next to the felspars, the commonest constituents of igneous rocks of almost all kinds, being especially characteristic of those of basic composition. An igneous rock composed almost wholly of pyroxene is known as a See also:pyroxenite. Besides being minerals of See also:primary origin in igneous rocks, the pyroxenes are also of frequent occurrence in metamorphic rocks, for example, in crystalline limestones, being then of secondary origin. At the See also:present See also:day the name pyroxene is used as a group name for all the minerals enumerated below, though sometimes it is also applied as a specific name to include the See also:monoclinic members See also:diopside, hedenbergite, schefferite and augite. Orthorhombic See also:Series. See also:Enstatite MgSiOi.

See also:

Bronzite (Mg,Fe)SiOi. See also:Hypersthene (Fe, Mg) SiOa. Monoclinic Series. Diopside CaMg(SiOa)2. Hedenbergite CaFe(SiOa)z. Schefferite (Ca,Mg) (Fe,Mn) (SiOa)2. Augite Ca(Mg,Fe)(SiO3)2with (Mg,Fe)(Al,Fe)2SiO6. Acmite NaFe ";SiOa)2. See also:Spodumene LiAl(SiO3)2. Jadeite NaAI(SiOa)2. See also:Wollastonite CaSiO3. Pectolite HNaCa2(SiO3)a.

Rosenbuschite Na2Caa[(Si,Zr,Ti)Oa]a. Anorthic Series. See also:

Rhodonite MnSiO3. Babingtonite (Ca,Fe,Mn)SiO8.Fe2"'(SiO3)a. Hiortdahlite (Ca,Na)2F[(Si,Zr)02]. For details respecting the See also:special characters and modes of occurrence of most of these species reference may be made to the respective headings: others not so treated are briefly mentioned below. Hedenbergite, or See also:calcium See also:iron pyroxene, is a black See also:mineral closely allied to diopside (q.v.) and, owing to the isomorphous replacement of iron by See also:magnesium, there is no See also:sharp See also:line of See also:division between them. Schefferite, or See also:manganese pyroxene, is a See also:brown mineral found in the manganese mines of See also:Sweden. Pectolite is a secondary mineral occurring as See also:white masses with a radially fibrous structure in the See also:veins and cavities of basic igneous rocks. Babingtonite is found as small black crystals on See also:felspar in the See also:granite of See also:Baveno in See also:Italy, and in the Haytor iron mine in See also:Devonshire. Rosenbuschite, hiortdahlite, and some other rare members containing See also:zirconium and See also:fluorine, occur as See also:accessory constituents in the nephelinesyenite of See also:southern See also:Norway.

End of Article: PYROXENE

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