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See also: mineral first observed in the 15th century at See also: Tolfa, near See also: Rome, where it is See also: mined for the manufacture of See also: alum
.
Extensive deposits are also worked in See also: Tuscany and Hungary, and at Bulladelah in New See also: South See also: Wales
.
By repeatedly roasting and lixiviating the mineral, alum is obtained in solution, and this is crystallized out by evaporation
.
See also: Alunite occurs as seams in trachytic and allied volcanic rocks, having been formed by the See also: action of sulphureous vapours on
these rocks
.
The See also: white, finely granular masses somewhat resemble
See also: 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 See also: 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 See also: 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 . |
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