Continental Drift Essay

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Theory of continental drift The hypothesis that the continents had once formed a single land mass before breaking apart and drifting to there present locations was first presented by Alfred Wenger. He believed that the continents were once joined in a super continent that scientists now call Pangaea. Over a vast period of time the continents drifted apart due to the earth’s rotation. In 1915 he published a book about his theory. His main evidence was the continents appear to have a jigsaw like fit, the west coast of Africa and South America have the same pattern of rock layers and have the same plant and animal fossils; some of these animals are only found in those parts of the world and their fossils show they could not swim. Although it had been noted that the shapes of the continents seemed to fit together Wenger died in 1930 and his ideas had still not been accepted. This was because there was no explanation for how the continents moved and because he was not a geologist. In the 1950s and years later geologists began to consider the theory of continental drift due to fossil records from separate continents showing the same species and mineral specimens along the same break lines of the continents. His ideas were not fully accepted until the 1960s when the Atlantic Ocean floor was surveyed in detail and the mid Atlantic ridge was discovered. This is a range of mountains and volcanoes in the middle of the ocean. Rock that was discovered on the ocean floor was found to be younger than the rock in the continents. The magnetic alignment of rocks containing iron rich minerals was symmetrical either side of the ridge. This new evidence fitted in with the theory of continental drift. Scientists also discovered that this movement could be caused by very powerful convection currents in the mantle. This brought about a new theory of plate tectonics. Scientists
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