Sadly, Wegener did not live to see the vindication of his theory, having died on an expedition to Greenland in 1930.
However, he had always been interested in. Wegener definition, German meteorologist and geophysicist: originated theory of continental. It was not until the 1960s that a mechanism would appear-the theory of plate tectonics, stating that the Earth's lithosphere is divided into plates on top of which the continents ride, slowly carried along by huge convection currents within the Earth's mantle. Born on November 1, 1880, Alfred Lothar Wegener earned a Ph.D in astronomy from the University of Berlin in 1904. Wegener attributed this to the movement of the poles followed the approximate path of the movement of his continents. Wegener's theory was soon rejected because he could not propose a suitable mechanism to account for the supposed drifting of continents. Alfred Wegener observed the apparent wandering of earths magnetic pole. In 1912, polar explorer and meteorologist Alfred Wegener first proposed the concept of continental drift, the geological theory that continents were once. As we’ve studied this idea over the decades, however, it has come to be the accepted theory of why our land areas are in their current location. The first truly detailed and comprehensive theory of continental drift was proposed in 1912 by Alfred Wegener, a German meteorologist.Bringing together a large mass of geologic and paleontological data, Wegener postulated that throughout most of geologic time there was only one continent, which he called Pangea. In the geological record he found corroborating evidence in the form of identical rock strata and fossil remains in eastern South America and western Africa and in other locations that would align if the continents fit together. Alfred Wegener’s continental drift theory faced fierce resistance initially, partially because of his outsider status, and partially due to his ideas of how the continents fit together. While on the expedition, Wegener constructed the first meteorological station in Greenland. In 1912 Alfred Wegener proposed a radical new idea, called continental drift, claiming that the primeval supercontinent (which he named Pangaea) had slowly broken apart, its pieces separating over millions of years into the locations observed today. Alfred Wegener was thrilled by this opportunity as he always dreamed of adventuring into an Artic climate because of the scientific and physical challenges. But they were unable to come up with a satisfactory model to explain how this giant landmass could become the modern continents positioned around the globe.
By the early twentieth century scientists observing this similarity speculated that the two continents must have once been joined together with the other continents as one large landmass. Biography A look at a map shows that the eastern coast of South America and the western coast of Africa have roughly the same outline.
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