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DANBURITE

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

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

End of Article: DANBURITE

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