What were Alfred Wegener accomplishments?
Alfred Wegener, in full Alfred Lothar Wegener, (born November 1, 1880, Berlin, Germany—died November 1930, Greenland), German meteorologist and geophysicist who formulated the first complete statement of the continental drift hypothesis. The son of an orphanage director, Wegener earned a Ph.
What were the three 3 pieces of evidence in support of Wegener’s theory?
The evidence for continental drift included the fit of the continents; the distribution of ancient fossils, rocks, and mountain ranges; and the locations of ancient climatic zones.
What is Alfred Wegener best known for?
Continental drift
Alfred Wegener/Known for
Wegener was a German meteorologist, geophysicist and polar researcher. In 1915 he published ‘The Origin of Continents and Oceans’, which outlined his theory of Continental Drift.
What are five facts about Alfred Wegener?
Alfred Lothar Wegener (1 November 1880 – 13 November 1930) was a German scientist and meteorologist. He is most notable for his theory of continental drift, which he proposed in December 1912….Alfred Wegener facts for kids.
| Quick facts for kids Alfred Wegener | |
|---|---|
| Known for | continental drift |
| Scientific career | |
| Fields | meteorology geology |
What are the 4 pieces of evidence for continental drift?
They based their idea of continental drift on several lines of evidence: fit of the continents, paleoclimate indicators, truncated geologic features, and fossils.
What are 6 pieces of evidence that support continental drift?
What are 2 interesting facts about Alfred Wegener?
Wegener began his work studying meteorology and physics before finally receiving a doctorate in astronomy in 1905. He and his brother Kurt pioneered the research that used weather balloons to track air currents, and at one point held the record for the longest continuous balloon flight at 52.5 hours.
Who was Alfred Wegener And what did he theorize?
Alfred Wegener was a German meteorologist who achieved fame for his theory of continental drift. This was a theory he put forth in 1912 that the continents had not always been in their present locations, but instead, drifted across the ocean towards and away from each other.
