The Earth Its Genesis And Revolution Considered in the Light of the Most Recen

Cover The Earth Its Genesis And Revolution Considered in the Light of the Most Recen
The Earth Its Genesis And Revolution Considered in the Light of the Most Recen
A T Swaine
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45. Folding in Cretaceous Zone of Swiss Alps. (A. Heim, Geol. Karie der Schweitz, N. F. , vol. Xvi. ) (See Fig. 47 for key. ) Fig. 46. Folded Strata pierced by Weissenstein Tunnel. (A. Baxtorf, Geol. Karte der Schweitz, N. F. , vol. Xxi. ) (See Fig. 47 for key. ) G r Wmgalle 3189 Fig. 47. Section across the Grosse Wingalle, about 7 miles, with inverted Jurassic Strata and involved Eocene. (A. Heim, Mech. Der Gebirgs- bildung, 1878. ) 1, Trias. 2, Lias. 3, Jurassic. 4, Tertiary. 5, Neoco- mian. ...6, Aptian. 7, Greensand. 8, Chalk. 9, Variegated Sandstone. 10, Red Clays. 11, Nummulite Limestone.
212 THE EARTH.
the heights of Asia -Minor, the Caucasus. Palestine, and the Himalayas, and onwards to Japan, received their principal plication and uplift in the Miocene and towards the close of the Pliocene period. The bed of the great Mediterranean Sea, which stretched as a belt round the heart of the Old World throughout the Cretaceous and earh T Tertiary epochs, was upheaved into a mountain system, and pro- duced some of the most remarkable physical features of the globe.


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