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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 .
Queen Louise Land and neighbouring areas NASA picture. Alfred Wegener in the Borg station during the 1912-1913 winter.. The Danish Expedition to Queen Louise Land, also known as the Danish expedition to Queen Louise Land and straight through Greenland’s ice sheet (Danish: Danske ekspedition til Dronning Louises Land og tværs over Nordgrønlands indlandsis), as well as Danish North Greenland ...
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.
This peninsula was named during the Three-year Expedition to East Greenland by Arne Noe-Nygaard (1908-1991). 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.
Earlier theories by Alfred Wegener and Alexander du Toit of continental drift postulated that continents in motion "plowed" through the fixed and immovable seafloor. The idea that the seafloor itself moves and also carries the continents with it as it spreads from a central rift axis was proposed by Harold Hammond Hess from Princeton University and Robert Dietz of the U.S. Naval Electronics ...
At a banquet held by the International Society for Arctic Research, the members toast scientist Dr. Carl Lorenz, about to recreate famed explorer Wegener's ill-fated expedition. Lorenz's team consists of two scientists, Dr. Johannes Brand and Dr. Jan Matushek, his friend, Fritz Kuemmel, their financial backer, John Dragan, and their pilot to ...
Alfred Wegener first proposed in 1915 that continents had once been joined together and had since moved apart. [ 6 ] [ 7 ] Although he produced an abundance of circumstantial evidence, his theory met with little acceptance for two reasons: (1) no mechanism for continental drift was known, and (2) there was no way to reconstruct the movements of ...
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.
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