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Alfred Lothar Wegener (/ ... After his return in 1908 and until World War I, Wegener was a lecturer in meteorology, ... three-part article [11] ...
Wegener said that of all those theories, Taylor's had the most similarities to his own. For a time in the mid-20th century, the theory of continental drift was referred to as the "Taylor-Wegener hypothesis". [26] [29] [30] [31] Alfred Wegener first presented his hypothesis to the German Geological Society on 6 January 1912. [5]
Alfred Wegener, around 1925 In 1912 Alfred Wegener proposed the theory of continental drift . [ 37 ] This theory suggests that the shapes of continents and matching coastline geology between some continents indicates they were joined together in the past and formed a single landmass known as Pangaea; thereafter they separated and drifted like ...
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]
BSc meteorologist Janice Davila tells Bored Panda that one of the most unknown facts from her field of expertise is that weather radars are slightly tilted upward in a half-degree (1/2°) angle.
It was led by German scientist Alfred Wegener (1880–1930), who had previously taken part in two other ventures to Greenland. His purpose was to make a systematic study of the Greenland ice sheet . In 1929, as a preliminary expedition ( German : Vorexpedition ), Wegener went to Greenland to explore a suitable place to reach the Greenland Ice ...
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Antonio Snider-Pellegrini (1802–1885) was a French geographer and geologist who theorized about the possibility of continental drift, anticipating Wegener's theories concerning Pangaea by several decades. In 1858, Snider-Pellegrini published his book, La Création et ses mystères dévoilés ("The Creation and its Mysteries Unveiled").