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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.
Among the scientists was German meteorologist Alfred Wegener. Georg Carl Amdrup was in charge of writing the official history of the expedition. In the autumn of 1906, northbound sled journeys began in order to lay depots along the route of the long northern explorations in the spring of the following year.
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.
In December 1938, Harrer married Lotte Wegener (1920–1989), the daughter of Alfred Wegener, German polar researcher and originator of the theory of continental drift. Her father had died on a Greenland expedition when she was 10. Their son Peter Harrer was born in December 1939, three months after Harrer was arrested by the British.
Fritz Loewe took part in the preparatory trip of the German Greenland Expedition led by Alfred Wegener in 1929. Working together with Ernst Sorge he became familiar with the newly-developed seismic procedure of measuring ice thickness. [3] In 1930-1931 he went back to Greenland to join the main expedition as a glaciologist.
As the temperature climbed to a record 128 degrees in Death Valley National Park, a group of motorcyclists was sickened by the heat, and one died. Motorcycle tour of Death Valley turns fatal as ...
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 F P f {\displaystyle F_{\mathrm {Pf} }} is that component of the centrifugal force during the rotation of the Earth that acts tangentially to the Earth's surface.