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My essay on Continental drift

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My essay on Continental drift
Theory of Continental Drift
The seven continents used to be one giant continent named Pangea. They spread apart and became what the continents are today. The shapes of the continents line up, the fossils line up with how the continents, the rock formations on both sides of the Atlantic line up with the fossils and coastlines, and climatic evidence proves the Theory of Continental Drift.
The first piece of evidence for Continental Drift is the shapes of the continents. All of the continents fit together I a logical way like a jigsaw puzzle. For example, South America and Africa fit together perfectly if you put them together. This is the same for all the other continents, but South America and Africa are the most obvious. Some of the continents traveled different distances or were flipped over the hundreds of millions of years that Continental Drift took place. In summary, the shapes of continents and how the coastlines fit together is a good piece of evidence for proving Continental Drift.
Another piece of evidence supporting the Theory of Continental Drift is the fossil evidence on both sides of the Atlantic Ocean. The rynchosaur is found on the west coast of Africa and the east coast of South America. This dinosaur is unable to swim, so it is not possible that it swam across the Atlantic Ocean. Clearly the best explanation for how the rynchosaur was found on both continents is that they were once one continent. Over all, fossil evidence proves that the Theory of Continental Drift is in fact true.
Yet another piece of evidence proving the Theory of Continental Drift is the rock formations on both sides of the Atlantic Ocean. The continents fit together in a certain way. In addition to the fossils proving that the continents fit together the way they do, the rock formations also prove this by corresponding with them. A good example of this is the basalt deposits connecting Europe and the top of Africa. The coastlines of the continents and how they fit together

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