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The Story of the development of the theory of Plate Tectonics The ideas developed between the 1930s and late 60’s represent a revolution in thinking about the Earth’s structure. At the time the theory caused lots of arguments among scientist. There is now overwhelming evidence for the theory of plate tectonics. Continental Drift to Plate tectonics The idea that continents can drift about is called, not surprisingly, Continental drift. This theory was developed by Alfred Wegener When Wegener first put forward the idea in 1912 people thought he idea was ridiculous. He believed that the continents were once joined forming a ‘supercontinent’ Pangaea, however the big problem was that he knew the continents had drifted but he couldn't explain how they drifted. The old theory before this time was the "Contraction theory" which suggested that the planet was once a molten ball and in the process of cooling the surface cracked and folded up on itself. Others thought that places like the Grand Canyon had been formed by a great catastrophe. The first idea to have a big impact came form Arthur Holmes in 1929. Holmes is widely regarded as the greatest British Earth Scientist of the 20th Century. Amongst his many contributions, he pioneered the study of the age of the Earth, using the radioactive decay of uranium to lead. He suggested that radioactive decay inside the Earth could produce heat which would set up convection currents in the mantle. The mantle behaves like ‘silly putty’ and can flow. This could be the driving force for the movement of the continents. 1940 Charles Richter mapped out the occurrence of earthquakes and noticed that they occurred in belts under volcanic ranges and in the oceans. (See CD tect.ppt) In the 1950s, oceanic exploration greatly expanded. Data gathered by oceanographic surveys conducted by many nations led to the discovery that a great mountain range on the ocean floor virtually encircled the Earth. (SEE CD Tect ppt.) Called the global mid-ocean ridge, this immense submarine mountain chain -- more than 50,000 kilometers (km) long and, in places, more than 800 km across -- zig-zags between the continents, The Story of the development of the theory of Plate Tectonics winding its way around the globe like the seam on a baseball. Rising an average of about 4,500 meters(m) above the sea floor, the mid-ocean ridge is nearly as high as Everest. Though hidden beneath the ocean surface, the global mid-ocean ridge system is the most prominent topographic feature on the surface of our planet. Magnetic striping and polar reversals (See CD Tect ppt) Later in the 1950s, scientists, using magnetic instruments (magnetometers) adapted from airborne devices developed during World War II to detect submarines, began recognizing odd magnetic variations across the ocean floor. Basalt -- the iron-rich, volcanic rock making up the ocean floor-- contains a strongly magnetic mineral (magnetite) and can locally distort compass readings. When the rock is formed it takes on the magnetic field direction prevailing at the time of formation. These newly discovered magnetic variations provided another means to study the deep ocean floor. 1962 Harry Hess 1963 Vine and Matthews Hess proposed that new ocean floor was made in the centres of oceans and then carried sideways on convection current conveyor belts. This became know as sea floor spreading. Fred Vine and Drum Matthews from Cambridge University realised that the magnetic stripes on either side of the ridge matched up. This provided convincing evidence that seafloor spreading was taking place Look at the animation on the CD. The Story of the development of the theory of Plate Tectonics 1965 J Tuzo Wilson. Proposed that the Earth is divided into several large rigid plates, these are moved apart as sea floors spread. See CD The Theory of Plate Tectonics 1967 Dan McKenzie at Cambridge University developed all the earlier ideas into the theory of plate tectonics. He calculated that the Earth’s circumference was not getting bigger, yet new crust was being developed by sea floor spreading in the oceans. He looked and found places were there was evidence that plates were being destroyed at the same rate. There is now overwhelming evidence for the theory of plat tectonics. Geologists now have a clear idea of what happens on Earth and many are looking for evidence of planets tectonics taking place on other planets. There is some evidence that Mars may not have plates. Astronomers have observed a huge volcano, several times the height of Everest, which suggests that the margins are static.