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Bøger af Jean Francois d'Aubuisson de Voisins

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  • af Jean Francois d'Aubuisson de Voisins
    448,95 kr.

    Le Trait����� de G�����ognosie V1 (1828) de De Voisins, Jean Fran�����ois D'Aubuisson, est un livre de r�����f�����rence en g�����ologie qui explore les diff�����rentes couches de la cro�����te terrestre et leur composition, ainsi que les processus g�����ologiques qui ont fa�����onn����� notre plan�����te. Il aborde �����galement les ph�����nom�����nes tectoniques et volcaniques, les formations g�����ologiques, les fossiles et la pal�����ontologie. Ce livre est une source pr�����cieuse d'informations pour les g�����ologues, les �����tudiants en g�����ologie et tous ceux qui s'int�����ressent ������ la science de la terre.This Book Is In French.This scarce antiquarian book is a facsimile reprint of the old original and may contain some imperfections such as library marks and notations. Because we believe this work is culturally important, we have made it available as part of our commitment for protecting, preserving, and promoting the world's literature in affordable, high quality, modern editions, that are true to their original work.

  • af Jean Francois d'Aubuisson de Voisins
    452,95 kr.

  • af Jean Francois d'Aubuisson de Voisins
    499,95 - 503,95 kr.

  • af Jean Francois d'Aubuisson de Voisins
    521,95 kr.

    Jean-Francois Daubuisson (1769-1841), geologist and engineer, was an Officer of the Legion d'Honneur, Knight of St Louis and Chief Engineer at the Royal Mining Corps. He published numerous papers on geology, mining and hydraulics, and is best known for his textbooks, Traite de geognosie and Traite d'hydraulique. He studied geology and mineralogy in Freiburg with Abraham Werner, the key proponent of Neptunism, the theory that all rocks had an aqueous origin. Later in his career Daubuisson was to side with the Plutonists, who argued that basalts formed from molten rock. However, in this paper, published in French in 1803, he describes his observations of the basalts of Saxony and argues that they, and all basalts, are sedimentary. This English translation by the Secretary of the Wernerian Natural History Society was published in 1814, and provides a fascinating insight into this discredited but once influential theory of the Earth.