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MISPICKEL
, a See also:mineral consisting of See also:iron sulpharsenide, FeAsS; it contains 46% of See also:arsenic, and is of importance as anore of this See also:element
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It is known also as arsenopyrite or arsenical See also:pyrites (Ger
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Arsenikkies) : mispickel is an old name of See also:German origin, and in the See also:form Mistpuckel was used by G
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See also: Mispickel is the See also:principal source of arsenious See also:oxide or the " white arsenic " of See also:commerce (see ARSENIC) . The See also:chief supplies are from Cornwall and Devon, and See also:Freiberg in See also:Saxony, and from See also:Canada and the See also:United States . Danaite is a cobaltiferous variety of mispickel, containing up to 9% of See also:cobalt replacing iron; it was first noticed by J . F . See also:Dana in 1824 at See also:Franconia in New See also:Hampshire . This variety forms a passage to the See also:species glaucodote, (Co,Fe)See also:AsS, which is found as well-See also:developed orthorhombic crystals in copper ore at Hakansboda in Ramberg See also:parish, Vestmanland, See also:Sweden . Other species belonging to this isomorphous See also:group of orthorhombic minerals are marcasite (FeS2), lollingite (FeAs2), safflorite (CoAs2) and rammelsbergite (NiAs2) . (L . J . |
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