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) (14755268866).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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97-105 et 145-157, pi. lll et V-VIl : cartesbathymétriques). (Voir aussi B. Helland-Hansen and F. Nansen, The Norwegian Sea, ilsPhysical Oceanography based upon the Norwegian Researches, 1900-190^ (Report on NorwegianFishery and Marine Investigations, H, n 2, Bergen, 1909, carte bathymétri(iue).) (2. On trouvera, sur la géologie et la cartographie du Spitzberg, les renseignementsles plus détaillés dans le recueil suivant : Swedish Explorations in Spitzbergen, 1758-1908.Ilistorical Sketch, by A. G. Nathorst; Swedish Spitzbergen Bibliography, by i. M. Hulth; SwedishSpitzbergen Maps, by G. De Geer (Yiner, Stockholm, XXIX, 1909, p. 3-89).J (3. Sur la région nord-occidentale du Spitzberg, formée de terrains anciens, et dont latopographie est au contraire vraiment alpestre, voir G. Isachsen, Spitsbergenekspeditionerne1906 (Det norske Geogr. Selsk. aarb. 1900-07, Kristiania). ln-8, 31 p., nombreuses photogr., Cj^ Profondeurs au. dfssus de 3ooo dp 3ooo à looo ^ de looo ^ à 200 ^de I
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0° Gr FiG .212. — Profondeurs du Bassin Polaire Arcti(iue, daprès F. Nansen (TheNorwegianNorthPolar Expédition. Scientific Results, vol. IV, 1904, a 13, pi. I). — Figure extraite duTraité de Géologie dÉm. Haug, I, 1907, p. 27, fig. G. Échelle l : 40 000 000 env. LAIJIIRNTIA ET ILES NORDIQUES. 945 sont situées entre les branches des Ouralides, et il est permis de consi-dérer le plateau comme un prolongement de la plaine de la )*etcliora*.La série stratigraphique, à partir du début des temps secondaires, res-semble non pas à celle de la province nord-atlantique, mais à celle desrégions polaires et du Pacilique septentrional. Ce quil y a de plusfrappant, cest que des coquilles marines tfe type miocène se rencontrentà la fois au Spitzberg et dans lEst du Groenland (I, p. 371 ; II, p. 106).Ce plateau est un champ de fractures; les îles les mieux connuessont coupées de failles, dans lesquelles la direction N.-S. domine^ La 2 cartes; Ad. Hoel, Geologiske iagltagelser p

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Suess, Eduard, 1831-1914;

Margerie, Emmanuel de, 1862-
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3 pt. 2
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29 July 2014



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