Evaluate the evidence that lead to the formation of the concept of which developed the theory of plate tectonics.

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Gary Woodsford         Geography        02/05/2007

Evaluate the evidence that lead to the formation of the concept of which developed the theory of plate tectonics.

        The earth is made up of 4 parts: Crust, Mantle, Outer core and the Inner core. The crust is compared to the earth a thin ‘skin’ it floats upon the mantle and is split into 2 different parts. The oceanic crust (sima) is a layer consisting mainly of basalt, averaging 6-10km in thickness, the continental crust (sial) can be 70km thick, and the crust is separated from the mantle by the Moho discontinuity. The crust and the rigid top layer of the mantle are collectively known as the lithosphere. The mantle is mainly composed of silicate rocks, rich in iron and magnesium. Apart from the top layer the rest of the rocks, the aesthenosphere, are kept in a semi-molten state. The mantle extends to a depth of 2900km where temperatures may reach 5000oC. These high temperatures form convection currents. The core consists of iron and nickel. The outer core is semi-molten while the inner core is solid; the temperature of the core, which is 6371km deep, is 5500oC.

Internal Structure of the Earth

        

The theory of plate tectonics was initially contrived by the work of 4 men, Francis Bacon, Alfred Wegener, Ewing and Hess.

        In 1620 Francis Bacon first realised that there was a resemblance between the west coast of Africa and the east coast of South America and he believed that these continents had once fit together like a jigsaw. Bacon’s theory was not taken seriously and had many problems due to the fact that it was only based on Bacon’s own vision of the world and the different continents. His theory was too subjective and it was difficult to prove. Later on other scientists could find better ways of showing that there was a similarity between different continents.

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        Later in 1912, a German meteorologist named Alfred Wegener published a theory that all the continents as known today were once joined into one super continent named Pangaea which split by unknown means and form 2 more continents named Laurasia and Gondwanaland which then split again to form today’s continents. Wegener collated evidence from several different sciences. He first said that the remains of a small reptile which lived in Permian times had been found in South Africa and South America, also a plant which existed when coal was being formed has also been located in India and Antarctica, also ...

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