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Plate Tectonics Theory

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PLATE TECTONICS THEORY

The theory of plate tectonics is widely accepted by scientists and it derived from the Continental Drift theory devised by Alfred Wegener. * In the 17th century is occurred to people that Africa and South America look as though they once fitted together. There were suggestions that the continents have moved apart. * In 1912, Alfred Wegener proposed the theory of continental drift. He suggested all continents were once joined as one supercontinent called ‘Pangaea’ which drifted apart. * He based the theory on geological evidence and fossils, but could not back it up with a mechanism explaining how the continents separated in the first place. * In the 1950’s palaeomagnetism provided evidence supporting continental drift. * In the 1960’s the process of seafloor spreading was discovered which provided a mechanism for continental drift. * The continental drift theory was further developed after these findings and became the foundations of plate tectonics theory.

Evidence for the theory:

Geology: - Areas of South America and Africa have rocks of the same age and composition. If you fit the continents together the distribution of the rocks match up. You can also match up the age, rock type and distribution of some mountain ranges. E.g. mountains in Scotland, Norway, Sweden and Finland are similar to those on the east coast of North America. These rocks and mountains must have formed under the same conditions and in the same place in order to match so well, which could only be possible if the continents were once joined.

Fossil records: - By fitting landmasses together, you can match up the distribution of some fossils. E.g. Fossils of Lystrosaurus, Cynognathus, Mesosaurus and Glossopteris. It is impossible that these species could have migrated across the earth, or that they have evolved in different

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