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But Wegener only published his idea after reading a paper in 1911 which criticised the prevalent hypothesis, that a bridge of land once connected Europe and America, on the grounds that this contradicts isostasy. [20] Wegener's main interest was meteorology, and he wanted to join the Denmark-Greenland expedition scheduled for mid-1912.
Wegener said that of all those theories, Taylor's had the most similarities to his own. For a time in the mid-20th century, the theory of continental drift was referred to as the "Taylor-Wegener hypothesis". [26] [29] [30] [31] Alfred Wegener first presented his hypothesis to the German Geological Society on 6 January 1912. [5]
In 1912 Alfred Wegener proposed the theory of continental drift. [36] This theory suggests that the shapes of continents and matching coastline geology between some continents indicates they were joined together in the past and formed a single landmass known as Pangaea; thereafter they separated and drifted like rafts over the ocean floor ...
Daniel Merton Wegner (June 28, 1948 – July 5, 2013) was an American social psychologist.He was a professor of psychology at Harvard University and a fellow of both the American Association for the Advancement of Science and the American Academy of Arts and Sciences.
Schematic distribution of fossils on Pangea according to Wegener. Moving on to the 20th century, Alfred Wegener introduced the Theory of Continental Drift in 1912, though it was not widely accepted until the 1960s. [4] This theory was revolutionary because it changed the way that everyone thought about species and their distribution around the ...
Alexander Logie du Toit FRS [1] (/ d uː ˈ t ɔɪ / doo-TOY; 14 March 1878 – 25 February 1948) was a geologist from South Africa and an early supporter of Alfred Wegener's theory of continental drift.
The root of this was Alfred Wegener's 1912 publication of his theory of continental drift, which was a controversy in the field through the 1950s. [2] At that point scientists introduced new evidence in a new way, replacing the idea of continental drift with instead a theory of plate tectonics. [2]
The German Greenland Expedition (German: Deutsche Grönlandexpedition), also known as the Wegener Expedition, was an expedition to Greenland in 1930–1931. It was led by German scientist Alfred Wegener (1880–1930), who had previously taken part in two other ventures to Greenland.