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) (14591532518).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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sifs reposesur celui qui lui fait suite à lOuest. La direction des plis reste la mêmeque celle des Alpes, mais chaque élément plonge en se dirigeant verslEst. Dans lAverser-Thal, les schistes des Grisons sappliquent contrele gneiss du Suretta ou le recouvrent. Ce gneiss repose à son tour sur (1. Voir L. Desbuissons, La Vallée de Binn (Valais). Étude géographique, géologique,minéralogiqne et pittoresque. In-8°, Lausanne, 1909, p. 23-46, 1 carte géol.. 1 pi. profils parH. Schardt). 2. Daprès F. M. Stapff (Ge/u^re/ies geologisches Profil in der Ehene des Goithardtunnels;Spezialbeilage zu den Quartalberichten des Schweizerischen Bundesralbes. In-P, 60 p., 1 pL,Zurich, 1880), la cuvette du Tessin est le résultat de ce plissement à rel)Ours; elle est méso-zoïque et renferme aussi des amphibolites. 3. Alb. Heim, Ûber die nordôstlichen Lappeii des Tessinermassives (Geol. Nachlese, Nr. 17;Vierteljahrsschr. d. Naturforscli. Gesellsch. Zurich, LL 1900, p. 397-402, pi. II). 1a^
Text Appearing After Image:
V V V .oV V > ^ V V V V X V AT^-v V*-^ / V V V -g V=: V vg €) v1,v\y= X> 5, V \ V ^ ; • M o O O I .M r^ --5 -O s «J : > c *j :s _^ Kl .ti 1^ ^ rt yî •- t- o rt O -^ f^ ► c c = M +S ■• îi ^ O (^ _w ^3 ^ 5 <; C ■ Cï ; ^ j a 2 ^. : —1 -; t- d (^ M ; ^ >t «-r ... -^ S 5 s 4 O te . rt 23 G -^ rt ^15 >^- M ^ X ^ - M 2 00 o C — ^ 2 ^ d -^ -;;;.;; sJ^pI ë Il ra co o -c3 ^ xî ,?>* ALPES 0 C GI D E N T A E E S . 731 une baiido iuésozoï((ii( qui a ôté suivie vers rauu)iit, dans la vallée duLiro, sur une vingtaine de kilouuties. (Test la ligne du Col du Spliïgen.Sous cette bande senfonce le gneiss du Massif du Tambo ; et celui-ciest supporté à lOuest par la bande mésozoïque du Val Mesocco, qui estégalement connue sur 20 kilomètres. Cest la ligne du Col de San Ber-nardino. Sous celle-ci plonge, du coté de lOuest, le Massif de lAdula;les dilîérentes masses gneissiques, ainsi que leur front, se sont graduel-lement déplacées v

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https://www.flickr.com/photos/internetarchivebookimages/14591532518/

Author

Suess, Eduard, 1831-1914;

Margerie, Emmanuel de, 1862-
Permission
(Reusing this file)
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Volume
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3 pt. 2
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Flickr posted date
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29 July 2014



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current18:16, 28 September 2015Thumbnail for version as of 18:16, 28 September 20153,088 × 2,240 (1.45 MB)SteinsplitterBot (talk | contribs)Bot: Image rotated by 90°
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