Siddhesh Joshi (Editor)

Auguste Michel Lévy

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Nationality
  
French

Fields
  
Geology

Influences
  
F Fouque

Name
  
Auguste Michel-Levy

Children
  
Albert Michel-Levy

Role
  
Geologist


Auguste Michel-Levy httpsuploadwikimediaorgwikipediacommonsthu

Institutions
  
Geological Survey of France

Died
  
September 27, 1911, Paris, France

Influenced by
  
Ferdinand Andre Fouque

Auguste Michel-Lévy (7 August 1844 – 27 September 1911) was a French geologist. He was born in Paris.

Biography

He became inspector-general of mines, and director of the Geological Survey of France. He was distinguished for his researches on extrusive rocks and their microscopic structure and origins. He employed the polarizing microscope early on for the identification of minerals. In his many contributions to scientific journals he described the granulite group, and dealt with pegmatites, variolites, eurites, the ophites of the Pyrenees, the extinct volcanoes of Central France, gneisses, and crystalline schists.

Auguste Michel-Lévy httpsuploadwikimediaorgwikipediacommonsbb

He wrote "Structures et classification des roches éruptives" (1889), but his more elaborate studies were carried out with Ferdinand André Fouqué. Together they wrote on the artificial production of feldspar, nepheline and other minerals, and also of meteorites, and produced "Minéralogie micrographique: roches éruptives françaises" (1879) and "Synthése des minéraux et des roches" (1882). Levy also collaborated with Alfred Lacroix in "Les Minéraux des roches" (1888) and "Tableau des minéraux des roches" (1889).

Michel-Lévy pioneered the use of birefringence to identify minerals in thin section with a petrographic microscope. He is widely known for the Michel-Lévy interference colour chart, which defines the interference colors from different orders of birefringence.

He also created classification schemes for igneous rocks which accounted for their mineralogy, texture, and composition, and showed that igneous rocks of different mineralogies could be formed from the same chemical composition, with different conditions of crystallization.

References

Auguste Michel-Lévy Wikipedia