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DANBURITE , a rare See also: mineral See also: species consisting of 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 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 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 granite at See also: Russell in St See also: Lawrence 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 Rhine) in See also: Switzerland
.
Splendid crystals have recently been obtained from See also: Japan
.
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