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: What’s going underneath our feet? Natural disasters rule the Earth, from Earthquakes to volcanic er uptions. How does this happen? For starters, the Earth’s crust known as the lithosphere is not just one big solid layer but is divided into large masses of land that has boundaries borders. These are called ‘tectonic plates’. (Farndon, 1998) The tectonic plate theory that has been acknowledged by Alfred Wegener who had in 1912 observed and concluded that continents could fit together like a jig-saw puzzle. (Kim Rutledge, Melissa McDaniel, Diane Boudeau, Tara Ramroop, Santani Teng, Erin Sprout, Hilary Costa, Hilary Hall, Jeff Hunt, n.d.)From that he created a notion, that in the past there was only one big land mass. Wegener named the term “Continental Drift” and believed it was the reason behind the changes of our continents. There are two types of plates – continental plates that are mostly made up of land and the oceanic plates that is typically sea water. (Farndon, 1998) These plates are still moving today without you even noticing but moved very slow and not only about a cm. (Farndon, 1998) (Seagrave, 2012) (Seagrave, 2012) Following Wegener’s jig -saw theory, the continents that were connected have similar geological and biological proof in the areas that were joined together. There were evidence of plant fossils, animal fossils and rock types. (Kim Rutledge, Melissa McDaniel, Diane Boudreau, Tara Ramroop, Santani Teng, Erin Sprout, Hilary Costa, Hilary Hall, Jeff Hunt, n.d.) E.g. South-East America and South Africa are the only to habitats that had evidence of the ancient reptile mesosaurus, to sum it all off the two lands had fit together. (Kim Rutledge, Melissa McDaniel, Diane Boudreau, Tara Ramroop, Santani Teng, Erin Sprout, Hilary Costa, Hilary Hall, Jeff Hunt, n.d.) When tectonics plates are either pulling or pushing (diverging and converging) new features can form. When two plates are converging, pushing towards each other they both collide and together go up. These converging movements can possibly result in producing new mountain ranges. (Tectonics, 2010) However, sometimes instead of pushing, they pull in opposite directions and consequently take lands apart. (Tectonics, Plate Boundaries, 2010) E.g. The Himalayas is an example of converging plates. (Monte Hieb, Nanch Hieb, n.d.) It was a result of the collision of the Eurasian plate and Indian Plate. (Tectonics, 2010) Some volcanoes are formed by an oceanic plate and a continental plate pushes towards each other, in this process the oceanic plate sinks underneath the continental plate that is pushes above. (Seagrave, 2012) When this occurs we call it the subduction zone. (Jessa, 2010) This is because the oceanic plate is denser than the continental plate. (Survey, 2008) E.g. the ‘Ring of Fire’ is an example of a subduction zone, it is an active area of earthquakes and volcanic activity. (Kim Rutledge, Melissa McDaniel, Diane Boudreau, Tara Ramroop, Santani Teng, Eric Sprout, Hilary Costa, Hilary Hall, Jeff Hunt, n.d.)
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