CRYOLITE
, a See also:mineral discovered in See also:Greenland by the Danes in 1794, and found to be a See also:compound of See also:fluorine, See also:sodium and See also:aluminium
.
From its See also:general See also:appearance, and from the fact that it melts readily, even in a See also:candle-See also:flame, it was regarded by the Eskimos as a See also:peculiar See also:kind of See also:ice; from this fact it acquired the name of cryolite (from Gr. icpboc, See also:- FROST (a common Teutonic word, cf. Dutch, vorst, Ger. Frost, from the common Teutonic verb meaning " to freeze," Dutch, vriezcn, Ger. frieren; the Indo-European root is seen in Lat. pruina, hoar-frost, cf. prurire, to itch, burn, pruna, burning coal, Sans
- FROST, WILLIAM EDWARD (1810–1877)
frost, and ki.See also:Bos, See also:- STONE
- STONE (0. Eng. shin; the word is common to Teutonic languages, cf. Ger. Stein, Du. steen, Dan. and Swed. sten; the root is also seen in Gr. aria, pebble)
- STONE, CHARLES POMEROY (1824-1887)
- STONE, EDWARD JAMES (1831-1897)
- STONE, FRANK (1800-1859)
- STONE, GEORGE (1708—1764)
- STONE, LUCY [BLACKWELL] (1818-1893)
- STONE, MARCUS (184o— )
- STONE, NICHOLAS (1586-1647)
stone)
.
Cryolite occurs in colourless or See also:snow-See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white cleavable masses, often tinted See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
brown or red with See also:iron See also:oxide, and occasionally passing into a See also:black variety
.
It is usually translucent, becoming nearly transparent on See also:immersion in See also:water
.
The mineral cleaves in three rectangular directions, and the crystals occasionally found in the crevices have a cubic See also:habit, but it has been proved, after much discussion, that they belong to the anorthic See also:system
.
The hardness is 2.5, and the specific gravity 3
.
Cryolite has the See also:formula Na3AIF6, or 3NaF•AlF3, corresponding to fluorine 54.4, sodium 32.8, and aluminium 12.8%
.
It See also:colours a flame yellow, through the presence of sodium, and when heated with sulphuric See also:acid it evolves hydrofluoric acid
.
Cryolite occurs almost exclusively at Ivigtut (sometimes written Evigtok) on the Arksut See also:Fjord in S.W
.
Greenland
.
There it forms a large See also:deposit, in a granitic vein See also:running through See also:gneiss, and is accompanied by See also:quartz, siderite, See also:galena, See also:blende, chalcopyrite, &c
.
It is also associated with a See also:group of kindred minerals, some of which are evidently products of alteration of the cryolite, known as pachnolite, thomsenolite, ralstonite, gearksutite, arksutite, &c
.
Cryolite likewise occurs, though only to a limited extent, at Miyask, in the Ilmen Mountains; at See also:Pike's See also:Peak, See also:Colorado, and in the Yellowstone See also:Park
.
Cryolite is a mineral of much economic importance
.
It has been extensively used as a source of metallic aluminium, and as a See also:flux in smelting the See also:- METAL
- METAL (through Fr. from Lat. metallum, mine, quarry, adapted from Gr. µATaXAov, in the same sense, probably connected with ,ueraAAdv, to search after, explore, µeTa, after, aAAos, other)
metal
.
It is largely employed in the manufacture of certain sodium salts, as suggested by See also:Julius See also:Thomsen, of See also:Copenhagen, in 1849; and it has been used for the See also:production of certain kinds of See also:porcelain and See also:glass, remarkable for its toughness, and for enamelled See also:ware
.
Although cryolite is known as ice-stone " (Eisstein), it is not to be confused with "ice-spar" (Eisspath), which is a vitreous kind of See also:felspar termed " glassy felspar" or
rhyacolite_ (F
.
W
.
End of Article: