Déodat Gratet de Dolomieu

Déodat Gratet de Dolomieu

Déodat Gratet de Dolomieu
Born 23 June 1750
Dolomieu
Died 28 November 1801 (1801-11-29) (aged 51)
Chateauneuf
Nationality France
Fields geology

Dieudonné Sylvain Guy Tancrède de Gratet de Dolomieu usually known as Déodat de Dolomieu (23 June 1750 – 28 November 1801) was a French geologist; the mineral and the rock dolomite and the largest summital crater on the Piton de la Fournaise volcano were named after him.

Biography and career

Déodat de Dolomieu was born in Dauphiné, France, one of 11 children of the Marquis De Dolomieu and his wife Marie-Françoise de Berénger. As a child young Déodat showed considerable intellectual potential and special interest in the natural surroundings of his home in the Alps of southeastern France. De Dolomieu began his military career in the Sovereign and Military Order of the Knights of Saint John (also called the Knights Hospitaller or the Knights of Malta) at the age of 12. His association with the Maltese Order caused him difficulties throughout his life, beginning with a duel, which he fought at the age of 18, when he killed a fellow member of the Order. For this infraction he was sentenced to life in prison but due to the intercession of Pope Clement XIII he was released after only 1 year.

During the years prior to the French Revolution De Dolomieu took full part in the intellectual ferment of France and the rest of Europe. He maintained numerous social contacts among the nobility and although he never married, De Dolomieu had something of a reputation as a ladies' man. Through his friend and mentor, the Duke de La Rochefoucauld, De Dolomieu was made a corresponding member of the Royal Academy of Sciences. He spent his spare time taking scientific excursions throughout Europe collecting mineral specimens and visiting mining areas. His particular interests included mineralogy, volcanology, and the origin of mountain ranges. Although De Dolomieu was greatly interested in volcanoes, he became convinced that water played a major role in shaping the surface of the Earth through a series of prehistoric, catastrophic events. De Dolomieu was not a uniformitarian geologist. His contemporary, James Hutton, did not publish the principle of uniformitarianism until 1795. De Dolomieu was an observationalist and spent much of his time collecting and categorizing geological data. Unlike Hutton, no scientific principles or theories are credited to him, although he left his permanent mark on geology in another way: that is by discovering the mineral that would be named after him.

During one of his voyages to the Alps of Tyrol (today part of northeastern Italy) De Dolomieu discovered a calcareous rock which, unlike limestone, did not effervesce with weak hydrochloric acid. He published these observations in 1791 in the well-known French science magazine "Journal de Physique". In March 1792, the rock was named dolomie (or dolomite, in English) by Nicolas-Théodore de Saussure.[1] Today both the rock and its major mineral constituent bear the name of De Dolomieu, as do the Dolomites, the mountain range of northeastern Italy. De Dolomieu was not the first to describe the mineral dolomite. Most probably it was Linnaeus, who was the first to note the fact that this rock resembled limestone but does not effervesce with dilute acid.[2] In his book "Oryctographia Carniola, oder physikalische Erdbeschreibung des Herzogthums Krain, Istrien und zum Theil der benachbarten Länder", published by J. G. I. Breitkopf, Leipzig in 1778, the Austrian naturalist Belsazar Hacquet also observed this distinction between limestone and a rock that Hacquet described as lapis suillus.[3][4] The two men met in Laibach in 1784, when De Dolomieu visited Sigmund Zois.[5] However, Hacquet was well aware of the fact that the description of a limestone that would not effervesce with acid (and therefore had to be different from normal limestone) by the famous Carolus Linnaeus in 1768 preceded his own. On p. 5 of the second volume of his "Oryctographia Carniola", which appeared in 1781, Hacquet stated that the white powder he had found near the town of Vorle ("unterm Teil der Oberkrain") a white powder that strongly resembled limestone but would not react with dilute hydrochloric acid, reminded him of the Marmor Tardum described by Linnaeus.

In addition to his scientific activities De Dolomieu continued to advance in rank in the Knights of Malta and was promoted to Commander in 1780. However, he continued to have difficulties as a result of his liberal political leanings which were unpopular among the conservative nobility who controlled the Order. De Dolomieu retired from active military service in 1780 to devote all of his time to travels and scientific work.

De Dolomieu was at first a strong partisan of the French Revolution, which began in 1789. However, the murder of his friend the Duc de la Rochefoucauld, a near-escape from the guillotine, and the beheading of several of his relatives, turned him against the revolution. During this time De Dolomieu became a supporter of Napoleon Bonaparte. In 1795, having lost his fortune in the revolution, De Dolomieu accepted the position of Professor of Natural Sciences at the École Centrale Paris and started to write the mineralogical section of the Encyclopédie Méthodique. The following year he was appointed Inspector of Mines and Professor at the École Nationale Supérieure des Mines de Paris, where his portrait still hangs in the library. His extensive mineral collection is today housed at the Muséum National d'Histoire Naturelle of Paris.

By 1798 De Dolomieu had developed an international reputation as one of the leading geologists in the world and was invited to join the scientific expedition accompanying Bonaparte's invasion of Egypt, as part of the natural history and physics section of the Institut d'Égypte. In March 1799 De Dolomieu became ill and was forced to leave Alexandria, Egypt for France. His ship, caught in a storm, sought refuge at the port of Taranto, Italy where De Dolomieu was made a prisoner of war. General Thomas-Alexandre Dumas, the father of Alexandre Dumas, the author, was also captured and held. The city was part of the Kingdom of the Two Sicilies, which was then at war with France. De Dolomieu had previously made a powerful enemy of the Grand Master of the Maltese Order when he helped negotiate the surrender of the island of Malta to Napoleon. The Grand Master denounced De Dolomieu and he was transferred to Messina, Sicily and imprisoned under horrible conditions, in solitary confinement, for the next 21 months.

The imprisonment of a world-famous scientist, under such conditions, was abhorrent to the intellectual community of Europe. Even the scientific community of England (who was at war with France) protested the confinement. Talleyrand, the French foreign minister, attempted to negotiate Dolomieus release through the Pope. Napoleon, who was First Consul of France at the time, felt that asking for such an intervention by the Pope would be dishonorable. The future Emperor's approach to the problem was more direct. In the spring of 1800 Napoleon led the French army into Italy, delivering a crushing blow to the Austrians and their Italian allies on 14 June at the Battle of Marengo. All of Italy then came within Napoleon's sphere. One of the terms dictated by Napoleon in the peace treaty of Florence (March 1801) was the immediate release of De Dolomieu.

Upon his liberation De Dolomieu resumed his scientific studies and field excursions. But his health, broken by the long imprisonment in Sicily, gave way during a trip to the Alps. Déodat de Dolomieu died on 28 November 1801 at the home of his sister at Châteauneuf.

Dr. George F. Kunz wrote about his contributions to mineralogy.[6][7]

References

  1. ↑ Saussure le fils, M de. (1792): Analyse de la dolomie. Journal de la Physique, vol.40, pp.161-173. Gardien, Guy (2002). "Introduction". Déodat Gratet de Dolomieu (in French). Editions Publibook. p. 9. ISBN 9782748312386.
  2. ↑ On p.41 of part 3 of his book "Systema naturae per regna tria naturae, Secundum Classes, Ordines, Genera, species cum characteribus & differentiis" published in 1768 by Laurentii Salvii, Homiae, 236 p., Linnaeus stated clearly: "Marmor tardum - Marmor particulis subimpalpabilius album diaphanum. Hoc simile quartzo durum, distinctum quod cum aqua forti non, nisi post aliquot minuta & fero, effervescens". In translation: "Slow marble - Marble, white and transparent with barely discernable particles. This is as hard as quartz, but it is different in that does not, unless after a few minutes, effervesce with "aqua forti""
  3. ↑ Felizardo, Alexandre. "Baltazar Hacquet (1739–1815)". Cavernas em Foco (in Portuguese). Bookess. p. 119. ISBN 9788562418938.
  4. ↑ Kranjc, Andrej (2006). "Balthasar Hacquet (1739/40-1815), the Pioneer of Karst Geomorphologists". Acta Carsologica 35 (2). ISSN 0583-6050.
  5. ↑ Šumrada, Janez (2001). "Žiga Zois in Déodat de Dolomieu". Kronika: časopis za slovensko krajevno zgodovino [The Chronicle: the Newspaper for the Slovenian History of Places] (in Slovenian and English) (Association of Slovenian Historical Societies, Section for the History of Places) 49 (1/2): 65–72. ISSN 0023-4923.
  6. ↑ Kunz, George F. “Déodat Dolomieu.” Science Monthly. Volume 8, pages 527–536. June, 1919. (Based on Alfred Lacroix. “Notice Historique sur Déodat Dolomieu,1750–1801.” 88 pages, portrait, 1918)
  7. ↑ Kunz, George F. “Un Manuscrit [sic] inédit de Dolomieu sur la Minéralogie du Dauphiné.” Science. Volume 50, number 373, pages 373–374. October 17, 1919.

Bibliography

Wikisource has the text of the 1911 Encyclopædia Britannica article Dolomieu, Déodat Guy Silvain Tancrède Gratet de.
This article is issued from Wikipedia - version of the Thursday, May 05, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.