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May 15, 2019 · Alfred Wegener (November 1, 1880–November 1930) was a German meteorologist and geophysicist who developed the first theory of continental drift and formulated the idea that a supercontinent known as Pangaea existed on the Earth millions of years ago.
Alfred Wegener (1880–1930) became internationally known for his heavily disputed theory of continental drift, which he formulated as early as 1912. Yet his exploration of Greenland, as well as his related work in glaciology and aerology, also makes up a considerable part of his multifarious scientific career as a meteorologist and geophysicist.
Apr 5, 2024 · 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.
Born on November 1, 1880, Alfred Lothar Wegener earned a Ph.D in astronomy from the University of Berlin in 1904. However, he had always been interested in geophysics, and also became fascinated with the developing fields of meteorology and climatology. During his life, Wegener made several key contributions to meteorology: he pioneered the use ...
Nov 20, 2015 · Alfred Wegener (1880–1930) was a leading explorer, geophysicist, and meteorologist from Germany, and pioneer in the exploration of Greenland ( 1 ). His seminal volume of meteorology ( 2) is universally considered a fundamental manual for this discipline and was long a reference text for students and specialists.
Wegener and his predecessors. Rejection of Wegener's theory, 1910s–1950s. The fixists. Road to acceptance. Modern evidence. See also. Citations. General and cited sources. External links. Continental drift is the hypothesis, originating in the early 20th century, that Earth's continents move or drift relative to each other over geologic time. [1] .
Apr 16, 2024 · plate tectonics, theory dealing with the dynamics of Earth ’s outer shell—the lithosphere —that revolutionized Earth sciences by providing a uniform context for understanding mountain-building processes, volcanoes, and earthquakes as well as the evolution of Earth’s surface and reconstructing its past continents and oceans.
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