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COPPERAS (Fr. couperose; Lat. cupri r...

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Originally appearing in Volume V07, Page 110 of the 1911 Encyclopedia Britannica.
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COPPERAS (Fr. couperose; See also:Lat. cupri See also:rosa. the See also:flower of See also:copper)  , See also:green See also:vitriol, or ferrous sulphate, FeSO4.7H2O, having a bluish-green See also:colour and an astringent, inky and somewhat sweetish See also:taste . It is used in See also:dyeing and tanning, and in the manufacture of See also:ink and of See also:Nordhausen sulphuric See also:acid or fuming oil of vitriol (see See also:IRON) . See also:COPPER-GLANCE, a See also:mineral consisting of cuprous sulphide, Cu2S, and crystallizing in the orthorhombic See also:system . It is known also as chalcocite, redruthite and vitreous copper (See also:German, Kupferglaserz of G . See also:Agricola, 1546) . The crystals have the See also:form of six-sided tables or prisms; the See also:angle between the See also:prism faces (lettered o in the figure) being 6o° 25' . When twinned on the prism planes o, as is frequently the See also:case, the crystals simulate hexagonal symmetry still more closely, as in the minerals arag- onite and See also:chrysoberyl . Twinning also takes See also:place according to two other See also:laws, giving rise to interpenetrating crystals with the basal planes (s) of the two individuals inclined at angles of 69° or 87° 56' respectively . The mineral also occurs as compact masses of considerable extent . The colour is dark See also:lead-See also:grey with a metallic lustre, but this is never very See also:bright, since the material is readily altered, becoming See also:black and dull on exposure to See also:light . The mineral is soft (H.=22) and sectile, and can be readily cut with a See also:knife, like See also:argentite; sp. gr . 5.7 .

Analyses agree closely with the See also:

formula Cu2S, which corresponds to 79.8% of copper; small quantities of iron and See also:silver are some-times See also:present . Next to chalcopyrite, copper-glance is the most important ore of copper . It usually occurs in the upper See also:part of the copper-bearing lodes, and is a secondary sulphide derived from the chalcopyrite met with at greater depths; sometimes, however, the two minerals are found together in the same part of the lodes . The best crystals are from St Just, St Ives, and See also:Redruth in See also:Cornwall, and from See also:Bristol in See also:Connecticut . Small crystals of See also:recent formation are found on See also:Roman See also:bronze coins in the thermal springs at Bourbonne-See also:les-Bains . Copper-glance readily alters to other minerals, such as See also:malachite, covellite, See also:melaconite and chalcopyrite . On the other See also:hand, it is found as pseudomorphs after chalcopyrite, See also:galena, and organic structures such as See also:wood; copper-glance pseudomorphous after galena preserves the cleavage of the See also:original mineral and is known as harrisite . Isomorphous with copper-glance is the orthorhombic mineral stromeyerite, a See also:double copper and silver sulphide, CuAgS, which occurs in abundance in the See also:Altai Mountains . (L . J .

End of Article: COPPERAS (Fr. couperose; Lat. cupri rosa. the flower of copper)
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COPPER (symbol Cu, atomic weight 63.1, H=1, or 63.6...
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