DIOPSIDE , an important member of the See also:pyroxene See also:group of See also:rock-forming minerals. It is a See also:calcium-See also:magnesium metasilicate, CaMg (SiO3)2, and crystallizes in the See also:monoclinic See also:system. Usually some See also:iron is See also:present replacing magnesium, and when this pre-dominates there is a passage to hedenbergite, CaFe(SiO3)2, a closely allied variety of monoclinic pyroxene. These are distinguished from See also:augite by containing little or no See also:aluminium. Diopside is colourless, See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white, See also:pale See also:green to dark green or nearly See also:black in See also:colour, the See also:depth of the colour depending on the amount of iron present. The specific gravity and See also:optical constants also vary with the chemical See also:composition; the sp. gr. of diopside is 3.2, increasing to 3.6 in hedenbergite, and the See also:angle of optical extinction in the See also:plane of symmetry varies between 38° and 47° in the two extremes of the See also:series, Crystals are usually prismatic in See also:habit with a rectangular See also:cross-See also:section as shown in the figure: the angle between the See also:prism faces m, parallel to which there are perfect cleavages, is 92° 50'.
Several varieties, depending on See also:differences in structure and
chemical composition, have been distinguished, viz. coccolite (from KoKKOS, a See also:grain), a granular variety; salite or sahlite, from See also:Sala in See also:Sweden; malacolite; See also:diallage; violane, a lamellar variety of a dark See also:violet-See also:blue colour; chrome-diopside, a See also:bright green variety containing a small amount of See also:chromium; and many others. Belonging to the same series with diopside and hedenbergite is a See also:manganese pyroxene, known as schefierite, which has the composition (Ca, Mg) (Fe, Mn) (SiO3)2.
Diopside is the characteristic pyroxene of metamorphic rocks, occurring especially in crystalline limestones, and often in association with See also:garnet and See also:epidote. It is also an essential constituent of some
pyroxene-granites, diorites and a few other igneous rocks, but the characteristic pyroxene of this class of rocks is augite. See also:Fine transparent crystals of a pale green colour occur, with crystals of yellowish-red garnet (hessonite) and See also:chlorite, in See also:veins traversing See also:serpentine in the See also:Ala valley near See also:Turin in See also:Piedmont: a crystal of this variety (" alalite ") is represented in the accompanying figure. These, as well as the See also:long, transparent, See also:bottle-green crystals from the Zillerthal in the Tyrol, have occasionally been cut as See also:gem-stones. See also:Good crystals have been found also at Achmatovsk near See also:Zlatoust in the Urals, Traversella near See also:Ivrea in Piedmont (" traversellite "), Nordmark in Sweden, See also:Monroe in New See also:York, See also:Burgess in See also:Lanark See also:county, See also:Ontario, and several other places: at Nordmark the large, rectangular black crystals occur with See also:magnetite in the iron mines. (L. J.
End of Article: DIOPSIDE
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