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Alfred Wegener was born in Berlin on 1 November 1880, the youngest of five children, to Richard Wegener and his wife Anna. His father was a theologian and teacher of classical languages at the Joachimsthalschen Gymnasium [ 6 ] and Berlinisches Gymnasium zum Grauen Kloster .
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.
He named it after German scientist Alfred Wegener (1880–1930), who had taken part in the 1906–08 Danmark Expedition and the 1912–13 Danish Expedition to Queen Louise Land led by J.P. Koch. Wegener died in 1930 on the Greenland ice sheet during the Wegener Expedition led by himself. [1]
Ernst Sorge was a member of Alfred Wegener's expedition. Together with Johannes Georgi he stayed in Eismitte from July 1930 to August 1931. Fritz Loewe stayed from October 1930 to May 1931. Sorge hand-dug a 15 m deep pit adjacent to his subterranean snow cave, which served as living quarters during the seven-month-long overwintering.
Arthur Holmes and Alfred Rittmann saw it right (Rittmann 1939). Only an outsider can have the overview, only an outsider sees the forest, not only the trees (Hellman 1998b, p. 145). But A. Wegener did not have the specialisation to correctly weight the quality of the geophysical data and the paleontologic data, and its conclusions.
Polflucht (from German, flight from the poles) is a geophysical concept invoked in 1922 by Alfred Wegener to explain his ideas of continental drift.. The pole-flight force is that component of the centrifugal force during the rotation of the Earth that acts tangentially to the Earth's surface.
Kurt Wegener (1878–1964), German polar explorer and meteorologist, brother of Alfred Mike Wegener (born 1946), American Major League Baseball pitcher Myrton O. Wegener (1917–1991), American farmer, businessman, and politician
The concept that the continents once formed a contiguous land mass was hypothesised, with corroborating evidence, by Alfred Wegener, the originator of the scientific theory of continental drift, in three 1912 academic journal articles written in German titled Die Entstehung der Kontinente (The Origin of Continents). [11]