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RHODONITE

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Originally appearing in Volume V23, Page 270 of the 1911 Encyclopedia Britannica.
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RHODONITE , a member of the See also:

pyroxene See also:group of minerals, consisting of See also:manganese metasilicate, MnSiO3, and crystallizing in the anorthic See also:system. It commonly occurs as cleavable to compact masses with a See also:rose-red See also:colour; hence the name, from the See also:Greek 1 YSov (a rose). Crystals often have a thick See also:tabular See also:habit; there are perfect cleavages parallel to the See also:prism faces with an See also:angle of 87° 312'. The hardness is 52-627 and the specific gravity 3.4-3.68. The manganese is often partly replaced by See also:iron and See also:calcium, which may sometimes be See also:present in considerable amounts; a greyish-See also:brown variety containing as much as 20% of calcium See also:oxide is called " bustamite " ; " fowlerite " is a zinciferous variety containing 7% of See also:zinc oxide. Rhodonite is a See also:mineral liable to alteration, with the formation of manganese carbonate, hydrous silicate or oxides. The compact material, which is cut and polished for ornamental purposes, is often marked in a striking manner by See also:veins and patches of these See also:black alteration products. At Syedelnikova, near See also:Ekaterinburg in the Urals, compact material of a See also:good colour occurs in a See also:clay-See also:slate and is extensively quarried: boulders of similar material found at Cummington ,in See also:Massachusetts (" cummingtonite f7) have also been worked as an ornamental See also:stone. In the iron and manganese mines at Pajsberg near Filipstadt and Langban in Vermland, See also:Sweden, small brilliant and translucent crystals (" pajsbergite ") and cleavage masses occur. Fowlerite occurs as large, rough crystals, somewhat resembling See also:pink See also:felspar, with See also:franklinite and zinc ores in granular See also:limestone at See also:Franklin See also:Furnace in New See also:Jersey.

End of Article: RHODONITE

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