File:La face de la terre (Das Antlitz der Erde). Traduit de l'allemand, avec l'autorisation de l'auteur et annotée sous la direction de Emm. de Margerie. Avec une préf. par Marcel Bertrand (1897) (14777859302).jpg

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Identifier: lafacedelaterredv3p2sues (find matches)
Title: La face de la terre (Das Antlitz der Erde). Traduit de l'allemand, avec l'autorisation de l'auteur et annotée sous la direction de Emm. de Margerie. Avec une préf. par Marcel Bertrand
Year: 1897 (1890s)
Authors: Suess, Eduard, 1831-1914 Margerie, Emmanuel de, 1862-
Subjects: Physical geography
Publisher: Paris A. Colin
Contributing Library: Robarts - University of Toronto
Digitizing Sponsor: University of Toronto

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t cartes);A. Spitz und G. Dyrenfurth, Anzeiger d. k. Akad. Wiss. Wien, 7 nov. 1907, p. 424-427. (3. Le renversement de la série cristalline vers le Nord est général dans cette bande de jonc-tion : J. BIaas,EmPrq/inmuordernPtfrfaie(Verhandl. k. k. Geol. Reichsanst., 1909, p. 197-199).) 4. W. Gûmbel, Das Auftreten kristallinischer Schiefer im Bettenschwanger Thaïe bei Hin-delang (Geogn. Jahreshefte, I, 1888, p. 170-172); pour une description pétrographique, voirIv. .\. Reiser, Ueber die Eruptivgesteine des Algdn (in Tschermak, Mineralog. Petrogr. Mittheil.,X, 1889, p. 500-548, pi. X). 5. Th. Lorenz, mém. cité, p. 71. 6. G. Steinmann, Geologische Beobachtangen in den Alpen, I (Berichte Naturforsch.Gesellsch. Freiburg i. B., X, 1900, p. 258, pl. I). ?84 LA FA(1E DE LA TERRE. Tout iespace comprenant les groupes de Davos, de la Silvretta, deVArlberg et les Alpes Calcaires flotte sur les nappes l&pontiennes. Cest unfragment occidental de la nappe austro-alpine. La distance du Lac
Text Appearing After Image:
Echelle 10 20 3o 4o K FiG. 167. — Répartition des Roches vertes dans la Suisse Orientale et les régions voisines,daprès G. Steinmann (Berichte der Natiirforsch. Gesellschaft zii Frcibiirg i. B., X, 1900,Taf. I, p. 21). l. Terrains autochtones et Nappes Helvétiques (Mollasse, Flysch, Crétacé, etc.); 2. Nappes Lépontienneset Austro-Alpines ; 3. Principau.x affleurements de roches éruptives basiques récentes (Ophiolites) :4. Ligne de contact anormal (charriage) entre les Nappes Lépontiennes ou Austro-Alpines et leFlysch; 5. Limite probable du Flysch tertiaire et des schistes mésozoïques. — Échelle de 1 : 1 000 000. de Sils, dans lEngadine, jusquà Oberstdorf en Bavière mesure plusde 120 kilomètres. Là, près dOberstdorf, se trouve, sous la nappeaustro-alpine, un liséré lépontien; et, au-dessous de ce liséré, le Flyschreprésente la série helvétique. ALPES ORIENTALES. 785 Kotliplelz, à ((iii revient le mérite davoir visé à une synthèse de;^)lus en plus vast

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