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) (14591623368).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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seignements deviennent moins sûrs. On sait peu dechose sur lArchipel Sverdrup. Le pays est bas, et Schei pense queles plissements ne se continuent pas dans ITle Heiberg. Lintérieur estinconnu. Le Trias de lEureka Sound consiste en une succession de schistes etde calcaires, avec de nombreux filons-couches, comme on en rencontresi fréquemment dans le Nord, à Verhkoïansk par exemple. Quant à lhypothèse suivant laquelle la plus grande partie de 1. E. Etheridge, Palaeontology of the Coasts of the Arctic Lands visited hy the late BritishExpédition (Quart. Journ. Geol. Soc. London, XXXIV, 1878, p. 568-639, pL XXV-XXIX). Ilfaut y ajouter les rema^iues de Th. Tschernyschew, Die obercarbonischea Brachiopoden desVrai iind des Timan (Mém. Comité Géol., Saint-Pétersbourg, XVI, 1902, n° 2, p. 690 et suiv.). 2. E. Kittl, Die Triasfossilien von lleiireka Sand (Report of the Second Norwegian ArcticExpédition in the « Fram », 1898-1902. No 7). In-8°, 44 p., 3 pi., Kristiania, 1907. 9^^
Text Appearing After Image:
FiG. 210. — Carte géologique des Terres dEllesmere et lleiberg (Archipel Polaire Nord-Américain), daprès P. Schei (in A. G. Nathorst, Report of the Second Norwegian ArcticExpédition in the « Fram » 1898-1902, n° 1, p. 5, fig. 1). Indications complémentaires daprèsla carte de A. P. Low. Tracé des côtes daprès G. Isachsen et 0. Sverdrup. 1. Archéen; 2. Cambrien et Silurien; 3. Dévonien; 4. Carbonifère; 5. Roches volcaniques; ô. Terrainssecondaires; 7. Tertiaire. — Échelle de 1 : 5 000 000. V? LAIRENTIA KT ILlvS NOUDIQrKS. 031 lArcliipel Sver(lrM;) a;)()(irtien(lrait au Trias, ou nv. peut invoquer ensa faveur ((uuii seul ai-guuieat : cest que Mac (^liutock a rencontré deslambeaux isolés de dépots jurassiques sur les cotes opposées delArchipel Parry (par exemple Harpoceras à la Pointe Wilkie, Terre duPrince Patrick, 7(5 20 de lat. N.). Cependant on ny a jamais encoretrouvé de Trias jusquà présent, et le substratum paraît être constituépar le Carbonifère ho

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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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