Online Encyclopedia

TETRADYMITE

Online Encyclopedia
Originally appearing in Volume V26, Page 670 of the 1911 Encyclopedia Britannica.
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TETRADYMITE  , a

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mineral consisting of
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bismuth telluride and sulphide, Bi2Te2S, also known as " telluric bismuth." Sometimes
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sulphur is absent and the formula is then Bi2Tea; traces of selenium are usually
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present . Crystals are
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rhombohedral, but are rarely distinctly
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developed; they are twinned together in groups of four; hence the name of the mineral, from the Greek, rerpaSupos, fourfold . There is a perfect cleavage parallel to the basal
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plane; and the mineral usually occurs in foliated masses of irregular outline . The colour is steel-grey, and the lustre metallic and brilliant . The mineral is very soft (H = 1) and marks paper; the specific gravity is 7.2 to 7.6 . It was first found, in 1815, at Telemarken in Norway; crystals are from Schubkau near Schemnitz in Hungary . It often occurs in
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quartz associated with native gold . Other
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species very similar to tetradymite, but with different formulae, are: joseite, from
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San Jose near Marianna in Brazil; grunlingite (Bi,SaTe), from Caldbeck Fells in Cumber-
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land; and wehrlite, from Hungary . (L . J .

End of Article: TETRADYMITE
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TETRAGRAMMATON (rerrapa, four; ypciµµa, letter)

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