Our Wandering Continents: An Hypothesis of Continental Drifting

Africa Alpine Andean Antarctica Arctic Argentina Asia Atlantic Australia basalts basin beds belt beneath block Brazil Caledonian Cape Carboniferous central climatic close coast compression continent Continental Drift Cretaceous crust crustal curve deformation deposits depth developed Devonian diastrophism direction Earth east eastern Greenland eclogite epoch erosion Europe facies faunas flora folding foredeep forms fracture furthermore geological geosyncline glacials Glossopteris Gondwana Gondwanide Graham Land granite Greenland Hercynian India Islands Isostasy isostatic Jurassic land late latter Laurasia limestones Lower Madagascar margin mass Mesozoic Miocene mountain movement Newfoundland North America north-western northern northwards ocean orogeny overthrusting Pacific Palæozoic paramorphic Patagonia peneplained Permian phases Pole postulated presumed region rift rocks rotation Sandstone Schuchert sediments sial side Silurian sima South southern southwards Spitzbergen Staub strata stretching structure sub-crust Suess tectonic tension Tertiary Tethys thickness tillite tion trending Triassic trough Upper Ural volcanic Wegener westerly western wide Zealand zone