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WILLIAM SMITH (1769-1839)

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Originally appearing in Volume V25, Page 270 of the 1911 Encyclopedia Britannica.
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WILLIAM See also:SMITH (1769-1839)  , See also:English geologist, appropriately termed " the See also:Father of English See also:geology," and known among his acquaintances as " Strata See also:Smith," was See also:born at See also:Churchill in See also:Oxfordshire on the 23rd of See also:March 1767 . Deprived of his father, an ingenious mechanic, before he was eight years old, he depended upon his father's eldest See also:brother, a See also:farmer at Over See also:Norton, who was but little pleased with his See also:nephew's love of See also:collecting " pundibs " (Terebratulae) and " See also:pound-stones " (the large Echinoid Clypeus, then frequently employed as a pound See also:weight by dairywomen), and with his propensity for See also:carving sundials on soft See also:brown " See also:oven-See also:stone " of his See also:neighbour-See also:hood . The See also:uncle was, however, better satisfied when the boy, after studying the rudiments of See also:geometry and See also:surveying, began to take See also:interest in the draining of See also:land; and there is no doubt that See also:William Smith profited in after See also:life by the See also:practical experience he gained with his relative . At the See also:age of eighteen he became assistant to See also:Edward See also:Webb, surveyor, of See also:Stow-on-the-Wold, and traversed the Oolitic lands of Oxfordshire and See also:Gloucestershire, the See also:Lias See also:clays and red marls of See also:Warwickshire and other districts, studying their varieties of strata and soils . In 1791 his observations at Stowey and High See also:Littleton in See also:Somersetshire first impressed him with the regularity of the stra+a . In 1793 he executed the surveys and levellings for the See also:line . `f the See also:Somers( t See also:Coal.See also:Canal, in the course of which he See also:con-firmed a previous supposition, that the strata lying above the coal were not See also:horizontal, but inclined in one direction—to the E.—so as to terminate successively at the See also:surface . On being appointed engineer to the canal in 1794 he was deputed to make 'a tour of observation with regard to inland See also:navigation . During this tour, which occupied nearly two months, he journeyed to See also:York and See also:Newcastle and returned through See also:Shropshire and See also:Wales to See also:Bath; he carefully examined the See also:geological structure of the See also:country, and corroborated his generalization of a settled See also:order of See also:succession in the strata . After residing for two or three years at High Littleton he removed in 1795 to Bath, and three years later See also:purchased a small See also:estate at Tucking See also:Mill, Midford, about 3 M. distant from the See also:city, where he engaged in the last duties he performed as See also:resident engineer to the Coal Canal (1708-1799) . His numerous journeys had, satisfied him of the practicability of making a See also:map to show the ranges of the different strata across See also:England, and in 1794 he coloured his first geological map—that of the vicinity of Bath . At this See also:time he made acquaintance with the Rev .

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Benjamin See also:Richardson (d . 1832), from .1796 See also:rector of Farleigh See also:Hungerford, who possessed a See also:good collection of See also:local fossils, but knew nothing of the See also:laws of stratification . He had a See also:sound knowledge of natural See also:history, and he greatly aided Smith in learning the names and true nature of the fossils, while Smith arranged his specimens in the order of the strata . By this new friend Smith was introduced to the Rev . See also:Joseph Townsend (i738-1816), rector of Pewsey, and on a notable occasion in 1799 Smith dictated his first table of See also:British Strata, written by Richardson and now in the See also:possession of the Geological Society of See also:London . It was headed Order of the Strata, and their imbedded Organic Remains, in the neighbourhood of Bath; examined and proved See also:prior to 1799 . In 1813 Townsend published, with due See also:acknowledgment, much See also:information on the English strata communicated by William Smith, in a See also:work entitled The See also:Character of See also:Moses established for veracity Its an historian, recording events from the Creation to the See also:Deluge . Meanwhile Smith was completing and arranging the data for his large Geological Map of England and Wales, with See also:part of See also:Scotland, which appeared in 1815, in fifteen sheets, engraved on a See also:scale of 5 m. to in . The map was reduced to smaller See also:form in 1819; and from this date to 1822 twenty-one See also:separate See also:county geological maps and several sheets of sections were published in successive years, the whole constituting a Geological See also:Atlas of England and Wales . Smith's collection of fossils was purchased in 1816-r818 by the British Museum . In 1817 a portion of the descriptive See also:catalogue was published under the See also:title of a Stratigraphical See also:System of Organized Fossils . Prior to this, in 1816, he commenced the publication of Strata Identified by Organized Fossils, with figures printed on See also:paper to correspond in some degree with the natural See also:hue of the sirata .

In this work (of which only four parts were published, 1816-1817) is exemplified the See also:

great principle he established of the See also:identification of strata by their included organic remains . In See also:January 1831 the Geological Society of London conferred on Smith the first See also:Wollaston See also:medal; on which occasion See also:Sedgwick in an eloquent address referred to Smith as " the Father of English Geology "; and the See also:government conferred upon him a' life-See also:pension of £See also:loo per annum . The degree of LL.D. he received from See also:Dublin, at the See also:meeting of the British Association in that city in 1835 . In 1838 he was appointed one of the commissioners to select See also:building-stone for the new Houses of See also:Parliament . The last years of his life were spent at Hackness (of which he made a good geological map), near See also:Scarborough, and in the latter See also:town . His usually robust See also:health failed in 1839, and on 28th See also:August of that See also:year he died at See also:Northampton . He was buried at St See also:Peter's See also:church, and a bust by See also:Chantrey was placed in the See also:nave . In 1891 the See also:earl of Ducie erected a See also:monument to his memory at his native See also:place, Churchill . His See also:Memoirs, edited by his nephew, See also:John See also:Phillips, appeared in 1844 .

End of Article: WILLIAM SMITH (1769-1839)
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