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Alfred Wegner: Continental Drift

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In 1915 Alfred Wegener first proposed the theory of continental drift. Wegner hypothesised that there was a gigantic super continent 200 million years ago (Pangaea). He stated that the Pangaea broke up into two smaller continents, which then separated into landmasses that look like our modern day countries. Wegner provided evidence such as the shape of the east coast of South America fits the west coast of Africa, like pieces in a jigsaw puzzle. He also stated that there were unusual violet quartzites found in both in Brazil and South Africa moreover, he stated that the form and pattern of the ancient fold mountains of northwest Scotland, Norway, eastern Greenland, northern new found land and the coast of new England are similar to suggest there was once a continuous mountain range. Lastly he suggested that there were rare leaf fossils found in South America, South Africa India and Australia. Wegener provided this evidence to prove that there was once a Pangaea that spilt up.

Despite the evidence Wegener provided critics did not accept his theory, as he was not a geologist, also that Iberian Peninsula prevents the neat fit of Europe into Africa and Spain and Portugal only fitted if they were turned around and lastly he had no evidence on the process of how the continents drifted apart.

In order to prove Wegener theory there was two types of evidence needed to shown first that supports that that the continents actually drifted and second, that shows that the movement of the plates had caused the drift.

Later on in the 1950s when people accepted that the sea levels have constantly changed then an even closer fit can be seen at 200 metres or 2000 metres below present-day sea level.

Moreover there was more evidence yielded by rocks. Violet quartzites occur both in Brazil and South Africa at locations, which the jigsaw would have been adjacent.
Furthermore

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