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Oct 19, 2023 · The theory of continental drift is most associated with the scientist Alfred Wegener. In the early 20th century, Wegener published a paper explaining his theory that the continental landmasses were “drifting” across the Earth, sometimes plowing through oceans and into each other.
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.
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.
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 ...
May 29, 2018 · In 1909 he began his university career at the Physical Institute in Marburg, where he pursued a systematic study of surfaces of discontinuity in the atmosphere: characteristic global levels at which sudden sharp temperature and pressure differences appeared both in cloud layers and in clear air.
Alfred Wegener (1880-1930) was a German scientist who specialized in meteorology and climatology. His knack for questioning accepted ideas started in 1910 when he disagreed with the explanation that the Bering Land Bridge was formed by isostasy and that similar land bridges once connected the continents [ 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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