TALC
, a See also:mineral which in its compact forms is known as steatite, or soapstone
.
It was probably the µayvitres A Wos of See also:Theophrastus, described as a 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 of silvery lustre, easily
cut
.
The word talc, sometimes written talk, is said to come from the Arabic talc, and not to be connected, as has been fancifully suggested, with the See also:Swedish talja, " to cut." Talc and See also:mica were confused by the older writers, and even at the See also:present See also:day mica is sometimes known in See also:trade as talc; whilst the See also:term was formerly applied also to foliated See also:gypsum
.
Talc is found occasionally in small hexagonal and rhombic plates, with perfect basal cleavage, and they are supposed to be See also:monoclinic
.
Talc often occurs in foliated masses, sometimes with a curved See also:surface, readily separating into thin very flexible, non-elastic laminae
.
The plates give a six-rayed percussion-figure
.
Talc has a hardness of only about r, and a specific gravity of from 2.6 to 2.8
.
Its extreme softness and its greasy feel are characteristic
.
The lustre on the cleavage See also:face is pearly, or sometimes silvery, and one of the old names of the mineral was stella terrae, while See also:German writers sometimes called it Katzensilber
.
The See also:colour is 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, See also:grey, yellow or frequently See also:green
.
The mineral has strong birefringence and a small optic axial See also:angle
.
Talc is a See also:magnesium silicate H2Mg3Si4O12
.
It is generally regarded as a hydrous silicate, but the See also:water is expelled only at a very strong See also:heat, and may therefore be regarded as basic
.
By the See also:action of heat the hardness of the mineral is greatly increased
.
Pseudomorphs are known after actinolite, See also:pyroxene, &c., and the mineral has probably been generally formed by the alteration of ferro-magnesian silicates
.
Talc occurs chiefly in crystalline See also:schists, usually associated with See also:chlorite, See also:serpentine and See also:dolomite
.
See also:Fine examples of See also:apple-green colour are found at See also:Mount Greiner, in the Zillerthal, See also:Tirol
.
Talc-schist is a foliated See also:rock composed chiefly of talc, generally associated with See also:quartz and See also:felspar; but all soapy schists are not necessarily talcose
.
The pearly micaceous constituent of the Alpine protogine is a See also:muscovite
.
The " steatites " of See also:Pliny was a stone resembling See also:fat, but other-See also:wise undescribed
.
Being easily cut, steatite has always been a favourite material with the See also:carver: it was used for See also:Egyptian scarabs and other amulets, which were usually coated with a See also:blue vitreous glaze; and it was employed for See also:Assyrian See also:cylinder-See also:seals and for other See also:ancient signets
.
By the See also:Chinese steatite is largely used for ornamental carvings, but many of their " See also:soap-stone " figures are wrought in a compact See also:pyrophyllite (q.v.), which is essentially different from talc
.
The name agalmatolite is often applied to the material of these figures, and was suggested by M
.
H
.
See also:Klaproth from the See also:Greek ayaXpa, " an See also:image." Pagodite is an old name for Chinese figure-stone
.
Ancient steatite carvings are found among the ruins of See also:Rhodesia
.
Steatite is usually a white, grey, greenish or 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 substance, occurring in See also:veins or nodular masses or in lenticular bedded deposits
.
Pseudomorphs after quartz and dolomite occur near Wunsiedel in See also:Bavaria
.
In some cases it is a product of the alteration of pyroxenic rocks, and the commercial mineral may be very impure
.
The ease with which steatite may be worked, coupled with its See also:power of resisting heat, has led to its employment for vessels for See also:household use, whence it is called " potstone "—the lapis ollaris of old writers
.
Among the uses of steatite may be mentioned its employment, especially in See also:America, for sinks, stoves, firebricks, See also:foot-warmers, tips for See also:gas-burners and electric switchboards: when ground it is used as a filler for See also:paper, for See also:leather-dressing, for covering See also:steam-pipes, as an ingredient in soap, for See also:toilet-See also:powder, for certain paints and as a lubricant
.
A fine granular steatite is used by tailors for marking See also:cloth under the name of " See also:French See also:chalk " or " See also:Spanish chalk." See also:Slate pencils are made of steatite and pyrophyllite; and in See also:Burma steatite pencils are used for See also:writing on See also:black paper
.
In the oxyhydrogen See also:flame, steatite has been fused and See also:drawn out into threads, like quartz-See also:fibres
.
Steatite and talc-schists are widely distributed, and have occasion-ally been used as See also:building stones
.
When first raised the stone is soft, but hardens on exposure
.
Soapstone from See also:Gudbrandsdal is used in the See also:cathedral of See also:Trondhjem in See also:Norway
.
Veins of steatite occur in the serpentine of the See also:Lizard See also:district in See also:Cornwall, and the mineral was used under the name of soap rock in the manufacture of the old See also:Worcester See also:porcelain
.
Among localities of steatite369
in the See also:British Isles mention may be made of Crohy See also:Head and Gartan near See also:Letterkenny in co
.
See also:Donegal, See also:Ireland; the See also:Shetland isles, the See also:Hebrides (See also:Harris) and Shiness in See also:Sutherland
.
In See also:North America the See also:distribution of the mineral is very extensive; localities of economic importance are near Gouverneur and elsewhere in St See also:- LAWRENCE
- LAWRENCE (LAURENTIUS, LORENZO), ST
- LAWRENCE, AMOS (1786—1852)
- LAWRENCE, AMOS ADAMS (1814–1886)
- LAWRENCE, GEORGE ALFRED (1827–1876)
- LAWRENCE, JOHN LAIRD MAIR LAWRENCE, 1ST BARON (1811-1879)
- LAWRENCE, SIR HENRY MONTGOMERY (1806–1857)
- LAWRENCE, SIR THOMAS (1769–1830)
- LAWRENCE, STRINGER (1697–1775)
Lawrence co., New See also:York; at Francestown in New See also:Hampshire; See also:Stockbridge, See also:Windsor co., See also:Vermont; Lynnfield, See also:Massachusetts; near See also:Lafayette, See also:Pennsylvania; See also:Albemarle, Amelia, See also:- BUCKINGHAM
- BUCKINGHAM, EARLS, MARQUESSES AND DUKES OF
- BUCKINGHAM, FIRST DUKE
- BUCKINGHAM, GEORGE VILLIERS, 1ST DUKE 0E1
- BUCKINGHAM, GEORGE VILLIERS, 2ND DUKE 0E1 (1628-1687)
- BUCKINGHAM, HENRY STAFFORD, 2ND DUKE OF3 (1454-1483)
- BUCKINGHAM, JAMES SILK (1786-1855)
Buckingham, See also:Fairfax and Fluvanna See also:cos., See also:Virginia; See also:Cherokee, See also:Moore and Swain cos., North Carolina; and in See also:- MURRAY
- MURRAY (or MORAY), EARLS OF
- MURRAY (or MORAY), JAMES STUART, EARL OF (c. 1531-1570)
- MURRAY (or MORAY), SIR ROBERT (c. 1600-1673)
- MURRAY, ALEXANDER STUART (1841-1904)
- MURRAY, DAVID (1849– )
- MURRAY, EUSTACE CLARE GRENVILLE (1824–1881)
- MURRAY, JAMES (c. 1719-1794)
- MURRAY, JOHN
- MURRAY, JOHN (1778–1820)
- MURRAY, LINDLEY (1745–1826)
- MURRAY, LORD GEORGE (1694–1760)
- MURRAY, SIR JAMES AUGUSTUS HENRY (1837– )
- MURRAY, SIR JOHN (1841– )
Murray co., See also:Georgia
.
A fibrous steatite from New York See also:state, used in the manufacture of paper, is known as agalite
.
Rensselaerite is a See also:wax-like talcose substance, passing into serpentine, from St Lawrence co., New York, named by E
.
See also:Emmons in 1837 after S
.
See also:Van See also:Rensselaer, of See also:Albany, N.Y
.
Beaconite is an asbestiform talc from See also:Michigan, named by L
.
W
.
Hubbard
.
The term pyrallolite was given by Nils G
.
See also:Nordenskiold to a mineral from See also:Finland, which appears to be talc pseudomorphous after pyroxene
.
Talcoid was K
.
F
.
See also:Naumann's name for a white lamellar mineral from near Pressnitz in Bohemia
.
A blue earthy mineral from near See also:Silver See also:City, New See also:Mexico, known locally as " native See also:ultramarine," is a magnesium silicate
.
See " '1ilr1c and Soapstone " in vol. ii. of Mineral Resources of the U.S
.
(See also:Washington, 1909), and J
.
H
.
See also:Pratt, " Economic Papers," No
.
3 of Geol
.
Surv. of N
.
Carolina (1900) ; also E
.
W
.
See also:Parker in 19th See also:Report of U.S
.
Geol
.
Surv
.
(1898) ; C
.
H
.
See also:Smyth, junior, The Fibrous Talc See also:Industry of St Lawrence Co., N.Y., in " Mineral Industry," vol. ix., for 1900; and G
.
P
.
See also:Merrill's Non-metallic Minerals (New York, 1904)
.
(F
.
W
.
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