History of Plate Tectonics
Continental Drift The hypothesis of how the continents were all once together and then split apart and drifted to their current location. classroomatsea.net
Early Thoughts Elie de Beaumont (1829) o Idea: Earth was contracting stress from this caused mountain building Eduard Suess o o Austrian geologist Idea that the southern continents formed a single giant continent called Gondwanaland (or Gondwana) Earliest idea of Earth crust was the continents were fixed and the ocean basins were ancient features
Alfred Wegener Born in Germany in 1880 Doctorate of astronomy in 1905 Served at the aeronautical observatory at Lindenberg. Was injured shortly after joining the German army in WWI After the war, he did research in meteorology in Hamburg, Germany, for German government. He was a professor of meteorology at the University of Graz in Austria from 1924 to 1930. 1915 published The Origin of Continents and Oceans o Introduced the idea of continental drift, the continents move. He went on 4 polar expeditions between 1906 and 1930. On the last of these expeditions, he visited Greenland to try to determine the thickness of the Greenland ice sheet and the rate of drift of Greenland. At the end of that expedition, he died while rescuing some colleagues.
Wegener s 1 st Idea Coastlines seemed to fit together, especially South America and Africa. One land mass called Pangaea Greek meaning all land Pangaea split into two separate continents: Gondwanaland (Gondwana) to the south and Laurasia to the north.
paralleldivergence.com yourdictionary.com
Animation clips http://www.youtube.com/watch?v=wauk94adxpa &safety_mode=true&persist_safety_mode=1&safe= active http://www.youtube.com/watch?v=zjvdr5fzd4w&f eature=related&safety_mode=true&persist_safety_ mode=1&safe=active http://www.youtube.com/watch?v=nybtnfn3nbo &feature=related&safety_mode=true&persist_safety _mode=1&safe=active
Wegener s 2 nd Idea Geological evidence Glacial deposits (tillites) Scraping marks from the ice sheets during the Late Paleozoic glaciation were found on southern Africa, Australia, South America, India and Antarctica suggested that all were connected near the South Pole.
Glacial Striation, scraping Ice sheets during the Late Paleozoic glaciation (now termed the Gondwana Ice Age) wrpsteacher.org thisoldearth.net
Wegener s 3 rd Idea Fossil evidence Similar plant and animal fossil from the Paleozoic time period in the southern continents and between North America and Europe
Alexander du Toit (around 1937) South African geologist Supported Wegener s ideas With geological evidence he put Gondwana near the South Pole and the Northern landmass (America, Greenland, Europe, and Asia) at the equator. Northern landmass named Laurasia Evidence coal deposits. Proved paleontological evidence Mesosaurus : Permian freshwater reptile occurred in rocks of the same age in both Brazil and South Africa. Freshwater can t survive in marine type environment, so how did it get from South Africa to Brazil without going through the ocean?
answersincreation.org cosscience1.pbworks.com
Wegener s Idea of how Continents move Earth s crust was made of two pieces Upper had low density (continent) Lower had high density (ocean basin) The upper piece ploughed through the denser crust piece.
Why Alfred Wegener s Ideas were accepted O Could not fine a convincing mechanism to explain how the continents moved. O Physicists convinced geologists that Earth s outer layers were too rigid for continental drift to occur. O Wrong on how fast the continents were moving
Arthur Holmes He suggested convection currents dragged the two halves of the original continent apart, with consequent mountain building in the front where the currents are descending, and the ocean floor development on the site of the gap, where the currents are acceding. He knew he couldn t fight the physicists ideas without an outside independent source of evidence to back up his hypothesis.