Online Encyclopedia

CELESTINE, or CELESTITE

Online Encyclopedia
Originally appearing in Volume V05, Page 600 of the 1911 Encyclopedia Britannica.
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CELESTINE, or CELESTITE  , a name applied to native strontium sulphate (SrSO4), having been suggested by the celestial blue colour which it occasionally presents . This colour has been referred to a trace of iron phosphate, but in some cases such an explanation appears doubtful . The
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mineral is usually colourless, or has only a delicate shade of blue . Celestine crystallizes in the orthorhombic
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system, being isomorphous with
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barytes (q.v.) . The angle between the prism faces is 76° 17' . The cleavage is perfect parallel to the basal pinacoid, and less marked parallel to the prism . Although celestine much resembles barytes in its
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physical properties, having for example the same degree of hardness (3), it is less dense, its specific gravity being 3.9 . Celestine is a less abundant mineral than barytes . It is, however, much more soluble, and occurs frequently in mineral waters . W . W . Stoddart showed that many
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plants growing on
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Keuper marls containing celestine near Bristol appropriated the strontium salt, and the metal could be detected spectroscopically in their ashes .

Celestine occurs in the Triassic rocks of

Britain, especially in
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veins and geodes in the Keuper marl in the neighbourhood of Bristol . At Wickwar and Yate in Gloucestershire it is worked for
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industrial purposes . Colourless crystals, of
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great beauty, occurin association with
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calcite and native
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sulphur in the sulphur deposits of Sicily, as at Girgenti .
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Fine blue crystals are yielded by the copper mines of Herrengrund, in Hungary; a dark blue fibrous form is known from
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Jena; and small crystals occur in flint at
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Meudon near Paris . Very large
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tabular crystals are found in
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limestone on Strontian Island in Lake
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Erie; and a blue fibrous variety from near Frankstown, Blair Co., Penn., is notable as having been the
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original celestine on which the
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species was founded by A . G . Werner in 1798 . Celestine is much used for the preparation of strontium
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hydrate, which is employed in refining beetroot
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sugar in Germany . The mineral is used also as a source of various salts of strontium such as the nitrate, which finds application in pyrotechny for the production of red fire . (F . W .

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