Online Encyclopedia

DIASPORE

Online Encyclopedia
Originally appearing in Volume V08, Page 169 of the 1911 Encyclopedia Britannica.
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DIASPORE  , a native

aluminium hydroxide, AlO(OH), crystallizing in the orthorhombic
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system and isomorphous with
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gothite and
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manganite . It occurs sometimes as flattened crystals, but usually as lamellar or scaly masses, the flattened
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surface being a direction of perfect cleavage on which the lustre is markedly pearly in character . It is colourless or greyish-white, yellowish, sometimes
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violet in colour, and varies from translucent to transparent . It may be readily distinguished from other colour-less transparent minerals, with a perfect cleavage and pearly lustre—mica,
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talc,
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brucite, gypsum—by its greater hardness of 62-7 . The specific gravity is 3.4 . When heated before the
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blowpipe it decrepitates violently, breaking up into white pearly scales; it was because of this
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property that the
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mineral was named diaspore by R . J . Hairy in 18or, from Stavreipew, " to scatter." The mineral occurs as an alteration product of
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corundum or emery, and is found in granular
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limestone and other crystalline rocks . Well-
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developed crystals are found in the emery deposits of the Urals and at Chester, Massachusetts, and in
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kaolin at Schemnitz in Hungary . If obtainable in large quantity it would be of economic importance as a source of alumina . (L . J .

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