Online Encyclopedia

ALUNITE, or ALUMSTONE

Online Encyclopedia
Originally appearing in Volume V01, Page 773 of the 1911 Encyclopedia Britannica.
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ALUNITE, or ALUMSTONE  , a
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mineral first observed in the 15th century at
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Tolfa, near Rome, where it is
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mined for the manufacture of
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alum . Extensive deposits are also worked in Tuscany and Hungary, and at Bulladelah in New South Wales . By repeatedly roasting and lixiviating the mineral, alum is obtained in solution, and this is crystallized out by evaporation . Alunite occurs as seams in trachytic and allied volcanic rocks, having been formed by the
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action of sulphureous vapours on these rocks . The white, finely granular masses somewhat resemble
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limestone in appearance, and the more compact kinds from Hungary are so hard and tough that they are used for millstones . Distinct crystals of alunite are rarely met with in cavities in the massive material; these are rhombohedra with interfacial angles of 9o° 50', so that they resemble cubes in appearance . Minute glistening crystals have also been found loose in cavities in altered rhyolite . The hardness is 4 and the specific gravity 2.6 . The mineral is a hydrated basic aluminium and potassium sulphate, KAl3(SO4)2(OH)5 . It is insoluble in
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water, but soluble in sulphuric acid . First called aluminilite by J . C .

Delametherie in 1797, this name was contracted by F . S .

Beudant in 1824 to alunite . (L . J .

End of Article: ALUNITE, or ALUMSTONE
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ALUMINIUM (symbol Al; atomic weight 27.0)
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ALUR (Lur, Luri, Lurem)

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