The Controversial Theory of Continental Drift by Alfred Wegener
TLDR Alfred Wegener proposed the theory of continental drift in 1910, but it was initially rejected by the scientific community. However, after his death, more evidence emerged in the 1950s that confirmed his larger point about the movement of continents, leading to the universal acceptance of his theory by geologists today.
Timestamped Summary
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Alfred Wegener proposed the theory of continental drift in 1910, suggesting that the continents were once joined and subsequently moved, but his idea was initially rejected by the scientific community.
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Alfred Wegener is best known for his contributions to geology and geophysics, particularly his observation that South America and Africa seemed to fit together like puzzle pieces, an idea that had been noticed by others before him.
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Alfred Wegener pieced together the continents and continental shelves into one giant continent called Pangea, and found additional evidence such as similarities in animals and tapeworms on different continents.
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Alfred Wegener presented his theory of Continental Displacement, later known as Continental Drift, in 1912, which included evidence such as similarities in plant species, geological formations, and the distribution of fossils across different continents.
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In 1922, when Alfred Wegener's book was translated into English, the geology community worldwide harshly criticized him, partly due to anti-German sentiment and the fact that he wasn't a trained geologist, with some accusing him of having delirious ravings and toying with evidence.
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After Alfred Wegener's death, more evidence started to emerge in the 1950s, including the discovery of paleomagnetism on the ocean floor, which provided strong evidence for continental drift, and the development of the plate tectonics theory, which explained how and why the continents moved.
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Alfred Wegener's theory of continental drift was not entirely correct, but his larger point about the movement of continents has been confirmed and is universally accepted by geologists today, highlighting the difficulty of accepting new scientific ideas.