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See also: born at See also: Metz, on the 25th of See also: June 1814, and educated at the Ecole Polytechnique in See also: Paris
.
At the age of twenty he had qualified as a See also: mining engineer, and in 1838 he was appointed to take See also: charge of the mines in the Bas-Rhin (See also: Alsace), and subsequently to be professor of See also: mineralogy and geology at the Faculty of Sciences, Strassburg
.
In 1859 he became engineer in chief of mines, and in 1861 he was appointed professor of geology at the museum of natural See also: history in Paris and was also elected member of the See also: Academy of Sciences
.
In the following See also: year he became professor of mineralogy at the 1 See also: cole See also: des Mines, and in 1872 director of that school
.
In 188o the See also: Geological Society of See also: London awarded to him the Wollaston medal
.
His published researches date from 1841, when the origin of certain tin minerals attracted his See also: attention; he subsequently discussed the formation of bog-iron ore, and worked out in detail the geology of the Bas-Rhin (1852)
.
From 1857 to 1861, while engaged in See also: engineering See also: works connected with the springs of Plombieres, he made a series of interesting observations on thermal See also: waters and their influence on the See also: Roman See also: masonry through which they made their exit
.
He was, however, especially distinguished for his long-continued and often dangerous experiments on the artificial production of minerals and rocks
.
He likewise discussed the See also: permeability of rocks by See also: water, and the effects of such infiltration in producing volcanic phenomena; he dealt with the subject of metamorphism, with the deformations of the See also: earth's crust, with earthquakes, and with the composition and See also: classification of meteorites
.
He died in Paris on the 29th of May 1896
.
His publications were: Etudes et experiences synthetiques sur le metamorphisme et sur la formation des roches cristallines (186o); Etudes synthetiques de geologie experimentale (1879); See also: Les Eaux souterraines a l'epoque actuelle (2 vols., 1887); Le Eaux souterraines aux epoques anciennes (1887)
.
the 11th of See also: February 1795
.
In 18o8 he went to Winchester, and in r810 he was elected to a demyship at MagdalenSee also: College, See also: Oxford, where the lectures of Dr Kidd first awakened in him a See also: desire for the cultivation of natural science
.
In 1814 he graduated with second-class honours, and in the next year he obtained the prize for the Latin essay
.
From 1815 to 1818 he studied See also: medicine in London and See also: Edinburgh
.
He took his M.D. degree at Oxford, and was a See also: fellow of the College of Physicians
.
In 1819, in the course of a tour through See also: France, he made the volcanic See also: district of See also: Auvergne a See also: special study, and his Letters on the Volcanos of Auvergne were published in The Edinburgh Journal, 1820-21
.
He was elected F.R.S. in 1822
.
By subsequent journeys in Hungary, Transylvania, See also: Italy, See also: Sicily, France and See also: Germany he extended his knowledge of volcanic phenomena; and in 1826 the results of his observations were given in,a See also: work entitled A Description of Active and See also: Extinct Volcanos (2nd ed., 1848)
.
In See also: common with Gay Lussac and See also: Davy, he held subterraneous thermic disturbances to be probably due to the contact of water with metals of the alkalis and alkaline earths
.
In See also: November 1822 Daubeny succeeded Dr Kidd as professor of chemistry at Oxford, and retained this See also: post until 1855; and in 1834 he was appointed to the chair of botany, to which was subsequently attached that of rural See also: economy
.
At the Oxford botanic garden he conducted numerous experiments upon the effect of changes in See also: soil, See also: light and the composition of the atmosphere upon vegetation
.
In 183o he published in the Philosophical Transactions a paper on the iodine and bromine of See also: mineral waters
.
In the following year appeared his Introduction to the Atomic Theory, which was succeeded by a supplement in 1840, and in 185o by a second edition
.
In 1831 Daubeny represented the See also: universities of See also: England at the first meeting of the See also: British Association, which at his See also: request held their next session at Oxford
.
In 1836 he communicated to the Association a report on the subject of mineral and thermal waters
.
In 1837 he visited the See also: United States, and acquired there the materials for papers on the thermal springs and the geology of See also: North See also: America, read in 1838 before the Ashmolean Society and the British Association
.
In 1856 he became president of the latter See also: body at its meeting at See also: Cheltenham
.
In 1841 Daubeny published his Lectures on See also: Agriculture; in 1857 his Lectures on Roman Husbandry; in 1863 See also: Climate: an inquiry into the causes of its differences and into its influence on See also: Vegetable See also: Life; and in 1865 an Essay on the Trees and Shrubs of the Ancients, and a See also: Catalogue of the Trees and Shrubs indigenous to See also: Greece and Italy
.
His last See also: literary work was the collection of his Miscellanies, published in two volumes, in 1867
.
In all his undertakings Daubeny was actuated by a See also: practical spirit and a desire for the See also: advancement of knowledge; and his See also: personal influence on his contemporaries was in keeping with the high character of his various literary productions
.
He died in Oxford on the 12th of See also: December 1867
.
See Obituary by.See also: John
See also: Phillips in Proceedings of Ashmolean See also: Soc., 1868
.
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