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SIR WILLIAM EDMOND LOGAN (1798-1875)

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Originally appearing in Volume V16, Page 867 of the 1911 Encyclopedia Britannica.
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SIR See also:WILLIAM EDMOND See also:LOGAN (1798-1875)  , See also:British geologist, was See also:born in See also:Montreal on the loth of See also:April 1798, of Scottish parents . He was educatea partly in Montreal, and subsequently at the High School and university of See also:Edinburgh, where See also:Robert See also:Jameson did much to excite his See also:interest in See also:geology . He was in a business See also:house in See also:London from 1817 to 183o . In 1831 he settled in See also:Swansea to take See also:charge of a colliery and some See also:copper-smelting See also:works, and here his interest in geology found abundant See also:scope . He collected a See also:great amount of See also:information respecting the See also:South See also:Wales See also:coal-See also:field; and his data, which he had depicted on the 1-in. See also:ordnance survey See also:map, were generously placed at the disposal of the See also:geological survey under See also:Sir H . T. de la Beche and fully utilized . In 184o See also:Logan brought before the Geological Society of London his celebrated See also:paper " On the See also:character of the beds of See also:clay lying immediately below the coal-seams of South Wales, and on the occurrence of coal-boulders in the See also:Pennant Grit of that See also:district." He then pointed out that each coal-seam rests on an under-clay with rootlets of Stigmaria, and he expressed his See also:opinion that the under-clay was the old See also:soil in which See also:grew the See also:plants from which the coal was formed . To confirm this observation he visited See also:America in 1841 and examined the coal-See also:fields of See also:Pennsylvania and Nova See also:Scotia, where he found the under-clay almost invariably See also:present beneath the seams of coal . In 1842 he was appointed to take charge of the newly established geological survey in See also:Canada, and he continued as director until 1869 . During the earlier years of the survey he had many difficulties to surmount and privations to undergo, but the See also:work was carried on with great tact and See also:energy, and he spared no pains to make his reports trustworthy . He described the Laurentian rocks of the Laurentian mountains in Canada and of the See also:Adirondacks in the See also:state of New See also:York, poinling out that they comprised an immense See also:series of crystalline rocks, See also:gneiss, See also:mica-schist, See also:quartzite and See also:limestone, more than 30,000 ft. in thickness . The series was rightly recognized as representing the See also:oldest type of rocks on the globe, but it is now known to be a complex of highly altered sedimentary and intrusive rocks; and the supposed oldest known fossil, the Eozoon described by Sir J .

W . See also:

Dawson, I See also:Lord) See also:Roberts . F.R.S. in 1851, and in 1856 was knighted . In the same See also:year he was awarded the See also:Wollaston See also:medal by the Geological Society of London for his researches on the coal-strata, and for his excellent geological map of Canada . After his retirement in 1869, he returned to See also:England, and eventually settled in South Wales . He died at See also:Castle Malgwyn in See also:Pembrokeshire, on the 22nd of See also:June 1875 . See the See also:Life, by B . J . See also:Harrington (1883) . (H . B .

End of Article: SIR WILLIAM EDMOND LOGAN (1798-1875)
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