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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]
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]
Six months later, on 12 May 1931, Wegener's skis were discovered. Expedition members built a pyramid-shaped mausoleum in the ice and snow, and Alfred Wegener's body was laid to rest. Wegener had been 50 years of age and a heavy smoker, and it was believed that he had died of heart failure brought on by overexertion.
I think best approach is separate sections that: 1) describe the observation, 2) describe the various theories, 3) discuss Wegener's theory (because it is the most notable of all the theories), and then 4) discuss why Wegener's theory was rejected (because that is, nowadays, its most notable aspect).
Marie Tharp was born on July 30, 1920, in Ypsilanti, Michigan, the only child of Bertha Louise Tharp, a German and Latin teacher, and William Edgar Tharp, a soil surveyor for the United States Department of Agriculture. [6]
But A. Wegener did not have the specialisation to correctly weight the quality of the geophysical data and the paleontologic data, and its conclusions. Wegener's main interest was meteorology, and he wanted to join the Denmark-Greenland expedition scheduled for mid 1912. So he hurried up to present his Continental Drift hypothesis. [2]
In 1912 Alfred Wegener proposed the theory of Continental Drift. [26] This theory suggests that the shapes of continents and matching coastline geology between some continents indicates they were joined in the past and formed a single landmass known as Pangaea; thereafter they separated and drifted like rafts over the ocean floor, currently ...
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. [2]