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JET (Fr. jais, Ger. Gagat)

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Originally appearing in Volume V15, Page 359 of the 1911 Encyclopedia Britannica.
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JET (Fr. jais, Ger. Gagat)  , a substance which seems to be a See also:peculiar See also:kind of See also:lignite or See also:anthracite; often cut and polished for ornaments . The word " See also:jet " probably comes, through O . Fr. jaiet, from the classical gagates, a word which was derived, according to See also:Pliny, from Gagas, in See also:Lycia, where jet, or a similar substance, was originally found . Jet was used in See also:Britain in prehistoric times; many See also:round barrows of the See also:Bronze See also:age have yielded jet beads, buttons, rings, armlets and other ornaments . The abundance of jet in Britain is alluded to by See also:Caius See also:Julius See also:Solinus (fl . 3rd See also:century) and jet ornaments are found with See also:Roman See also:relics in Britain . Probably the See also:supply was obtained from the See also:coast of See also:Yorkshire, especially near See also:Whitby, where nodules of jet were formerly picked up on the See also:shore . Caedmon refers to this jet, and at a later date it was used for See also:rosary beads by the monks of Whitby See also:Abbey . The Whitby jet occurs in irregular masses, often of lenticular shape, embedded in hard shales known as jet-See also:rock . The jet-rock See also:series belongs to that See also:division of the Upper See also:Lias which is termed the See also:zone of See also:Ammonites serpentinus . Microscopic examination of jet occasionally reveals the structure of coniferous See also:wood, which A . C .

See also:

Seward has shown to be araucarian . Probably masses of wood were brought down by a See also:river, and drifted out to See also:sea, where becoming See also:water-logged they sank, and became gradually buried in a See also:deposit of See also:fine mud, which eventually hardened into shale . Under pressure, perhaps assisted by See also:heat, and with exclusion of See also:air, the wood suffered a peculiar kind of decomposition, probably modified by the presence of See also:salt water, as suggested by See also:Percy E . Spielmann . Scales of See also:fish and other fossils of the jet-rock are frequently impregnated with bituminous products, which may replace the See also:original tissues . Drops of liquid See also:bitumen occur in the cavities of some fossils, whilst inflammable See also:gas is not uncommon in the jet-workings, and See also:petroleum may be detected by its See also:smell . See also:Iron See also:pyrites is often associated with the jet . Formerly sufficient jet was found in loose pieces on the shore, set See also:free by the disintegration of the cliffs, or washed up from a submarine source . When this supply became insufficient, the rock was attacked by the jet-workers; ultimately the workings took the See also:form of true mines, levels being driven into the shales not only at their outcrop in the cliffs but in some of the inland dales of the Yorkshire See also:moor-lands, such as Eskdale . The best jet has a See also:uniform See also:black See also:colour, and is hard, compact and homogeneous in texture, breaking with a conchoidal fracture . It must be tough enough to be readily carved or turned on the See also:lathe, and sufficiently compact in texture to receive a high See also:polish . The final polish was formerly given by means of See also:rouge, which produces a beautiful velvety See also:surface, but rotten-See also:stone and lampblack are often employed instead .

The softer kinds, not capable of being freely worked, are known as See also:

bastard jet . A soft jet is obtained from the estuarine series of the See also:Lower Oolites of Yorkshire . Much jet is imported from See also:Spain, but it is generally less hard and lustrous than true Whitby jet . In Spain the See also:chief locality is See also:Villaviciosa, in the See also:province of See also:Asturias . See also:France furnishes jet, especially in the See also:department of the See also:Aude . Much jet, too, occurs in the Lias of See also:Wurttemberg, and See also:works have been established for its utilization . In the See also:United States jet is known at many localities but is not systematically worked . Pennsylvanian anthracite, however, has been occasionally employed as a substitute . In like manner Scotch cannel See also:coal has been sometimes used at Whitby . Imitations of jet, or substitutes for it, are furnished by vulcanite, See also:glass, black See also:obsidian and black See also:onyx, or stained See also:chalcedony . Jet is sometimes improperly termed black See also:amber, because like amber, though in less degree, it becomes electric by See also:friction . See P .

E . Spielmann, " On the Origin of Jet," Chemical See also:

News (Dec . 14, 1906) ; C . See also:Fox-Strangways, " The See also:Jurassic Rocks of Britain, Vol . I . Yorkshire," Mem . Geol . Sure . (1892); J . A . See also:Bower, " Whitby Jet and its Manufacture," Journ . See also:Soc .

Arts (1874, vol. xxii. p . 8o) .

End of Article: JET (Fr. jais, Ger. Gagat)
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