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Some truly revolutionary scientific theories may take years or decades to win general acceptance among scientists. This is certainly true of plate tectonics, one of the most important and far-ranging geological theories of all time; when first proposed, it was ridiculed, but steadily accumulating evidence finally prompted its acceptance, with immense consequences for geology, geophysics, oceanography, and paleontology. |
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He first presented his hypothesis in 1912. In 1915, he published “The Origin of Continents and Oceans, ” which contained his theory on continental drift |
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A ground-breaking hypothesis that explained how continents move across the surface of the Earth. Decades later, parts of Wegener's theories were validated by scientists and are now a part of the well recognized theory of plate tectonics. |
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The concept of shifting continents was first presented to geoscience by Wegener's continental drift theory. He suggested that before fragmenting into multiple distinct continents, Earth must have been a single supercontinent |
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This clarified how fossilized plants and animals as well as comparable rock formations could coexist on different continents. In accordance with Wegener's theory, modern science acknowledges that the ancient supercontinent Pangaea existed before disintegrating some 200 million years ago. |
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Jigsaw Fit, Geological Fit, and Tectonic Fit |
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Proof of Continental Drift Theory |
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More evidence comes from glacial striations – scratches on the bedrock made by blocks of rock embedded in the ice as the glacier moves. These show the direction of the glacier, and suggest the ice flowed from a single central point. |
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Wegener suggested that although the species had coexisted, the lands had separated once they had died and turned into _____ |
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Wegener proposed that all continents were once part of a single landmass or supercontinent called the _____ |
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emerged as evidence supporting Wegener’s theory long after his time. It refers to the study of the Earth's magnetic field as recorded in rock |
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Paleomagnetic studies revealed that the Earth's magnetic poles have reversed many times. These patterns, seen in rocks on either side of mid-ocean ridges, show symmetrical magnetic striping, providing evidence for seafloor spreading. |
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Studies of ancient magnetic fields suggested continents have moved over time, supporting the idea of continental drift. That polarwandering curves for different continents do not agree was one of the first important evidences for continental drift (the large-scale movements of continents and ocean basins relative to one another over geologic time). |
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