Léonce Élie de Beaumont | |
|---|---|
Léonce Élie de Beaumont | |
| Born | Jean-Baptiste Armand Louis Léonce Élie de Beaumont 25 September 1798 (1798-09-25) |
| Died | 21 September 1874 (1874-09-22) (aged 75) Canon, Calvados, France |
| Alma mater | École des mines |
| Awards | Wollaston Medal(1843) |
| Scientific career | |
| Fields | geology |
Jean-Baptiste Armand Louis Léonce Élie de Beaumont (25 September 1798 – 21 September 1874) was aFrenchgeologist.
Élie de Beaumont was born atCanon, inCalvados. He was educated at theLycee Henri IV where he took the first prize inmathematics andphysics at theÉcole polytechnique, where he stood first at the exit examination in 1819; and at theÉcole des mines (1819–1822), where he began to show a decided preference for the science with which his name is associated. In 1823 he was selected along withDufrénoy byBrochant de Villiers, the professor of geology in the École des Mines, to accompany him on a scientific tour toEngland andScotland, in order to inspect the mining and metallurgical establishments of the country, and to study the principles on whichGeorge Bellas Greenough's geological map of England (1820) had been prepared, with a view to the construction of a similar map of France.[1]
In 1835 he was appointed professor of geology at the École des Mines, in succession to Brochant de Villiers, whose assistant he had been in the duties of the chair since 1827. He held the office of engineer-in-chief of mines in France from 1833 until 1847, when he was appointed inspector-general; and in 1861 he became vice-president of the Conseil-General des Mines and a grand officer of theLegion of Honour. His growing scientific reputation secured his election to the membership of theAcademy of Berlin, of theFrench Academy of Sciences,[1] of theRoyal Society of Edinburgh (1845),[2] of theRoyal Society of London, as a foreign member of theRoyal Swedish Academy of Sciences (1848), and as an international member of theAmerican Philosophical Society (1860).[3] By a decree of the president he was made a senator of France in 1852, and on the death ofFrançois Arago in 1853 he was chosen as perpetual secretary of the Academy of Sciences.[1]
Élie de Beaumont's name is widely known to geologists in connection with his theory of the origin ofmountain ranges, first propounded in a paper read to the Academy of Sciences in 1829, and afterwards elaborated in hisNotice sur le système des montagnes (3 volumes, 1852). According to his view, all mountain ranges parallel to the same great circle of the earth are of strictly contemporaneous origin, and between the great circles a relation of symmetry exists in the form of a pentagonal réseau.[4] An elaborate statement and criticism of the theory was given in his anniversary address to theGeological Society of London in 1853 byWilliam Hopkins. The theory did not find general acceptance, but it proved of great value to geological science, owing to the extensive additions to the knowledge of the structure of mountain ranges which its author made in endeavouring to find facts to support it.[1]
Mount Elie de Beaumont is in theWestland Tai Poutini National Park, on thewest coast ofNew Zealand's theSouth Island and near the boundary withAoraki / Mount Cook National Park. It is 3109m high.
Probably the best service Élie de Beaumont rendered to science, however, was in connection with the geological map of France, in the preparation of which he had the leading share. During this period Élie de Beaumont published many important memoirs on the geology of the country. After his retirement from the École des Mines he continued to superintend the issue of the detailed maps almost until his death, which occurred at Canon. His academic lectures for 1843-1844 were published in 2 volumes, (1845–1849), under the titleLeçons de Géologie pratique.[5]