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) (14591613367).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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et des failles dans la Basse-Bourgogne(BulL Soc. GéoL de Fr., 4« sér., IV, 1904, p. 561-568, pi. XV : carte). 2. M. Bertrand, Sur la continuité du phénomène de plissement dans le Bassin de Paris (Bull.Soc. Géol. de Fr., 3 sér., XX, 1892, p. 118-165, pi. V, cartes dans le texte); voir aussi sa note :Lignes directrices de la Géologie de la France (C. R. Acad. Se, CXVIII, 1894, V sern.,p. 258-262.carte de la p. 260). 3. L. van Werveke, Uebersichtskarte der Veriuerfungen des mesozoischen Gebirges in Loth-ringen, Luxemburg und den angrenzenden Gebietender Rheinprovin: (in : Schumacher, Steinmannund van Werveke, Erlauterungen zur geologischen Uebersichtskarte des westlichen Deutsch-Lothringen. ln-8°, Strassburg, 1887, pl. II): ibid., p. 10, 11 : « Le Trias et le Jurassique... sesont effondrés tout autour des terrains anciens ». 4. D. P. OEhlert et A. Bigot, Note sur le Massif silurien dHesloup (Bull. Soc. Géol. de Fr.,3* sér., XXVI, 1898, p. 82-103, carte de la p. 83). I j y^
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> I ARMORIQUE ET ALTAIDES AMERICAINES. 617 Quon imagine maintenant que ce plissement posthume augmente(lintensité vers le Xord, conformément à la direction si nettement mar-quée dans le Sud de lAngleterre, quil englobe de petits horsts etquil soit arrêté par les Malvern Hills et leur prolongement nord-orien-tal alTaissé, et lon assistera, dans ces hautes montagnes inachevées, àune scène de lévolution des Alpes elles-mêmes. AltaïdesTransatlantiques. — De la rive méridionale du l.ac Majeurau bord externe du Jura, au Sud de Bàle, la distance est do 210à 220 kilomètres. Si on laisse de coté le Jura et la dépression de laMollasse, la largeur, de C.ôme à lanticlinal mollassique de Lucerne,devient de 190 à 200 kilomètres. De Bergame à Bregenz, on mesureapproximativement 200 kilomètres; mais une bande dinarique estencore comprise dans ce total. Une ligne menée suivant le méridien de 3 30 de long. W.transversalement à larc armoricain, depuis les roches à glauc

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