Online Encyclopedia

DANBURITE

Online Encyclopedia
Originally appearing in Volume V07, Page 793 of the 1911 Encyclopedia Britannica.
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DANBURITE  , a rare

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mineral
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species consisting of calcium and boron orthosilicate, CaB2(SiO4)2, crystallizing in the orthorhombic
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system . It was discovered by C . -U . Shepard in 1839 at
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Danbury,
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Connecticut, U.S.A., and named by him after this locality . The crystals are prismatic in habit, and closely resemble
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topaz in form and interfacial angles . There is an imperfect cleavage parallel to the basal
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plane . Crystals are transparent to translucent, and colourless to pale yellow; hardness 7; specific gravity 3•o . At Danbury the mineral occurs with
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microcline and
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oligoclase embedded in
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dolomite . Large crystals, reaching 4 in. in length, have been found with
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calcite in
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veins traversing granite at Russell in St Lawrence county, New York . Smaller but well-
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developed crystals have been found on
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gneiss at Mt . Scopi and Petersthal (the valley of the Vals Rhine) in
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Switzerland . Splendid crystals have recently been obtained from
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Japan .

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