Survey
* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project
PLATE TECTONICS Plate Tectonics • The Theory of Plate Tectonics states that the surface of the earth is broken up into a few large plates and many smaller ones Plate Tectonics Plate Tectonics • These solid plates float on the semisolid mantle • The plates interact with each other in three major ways: – Pull away from each other “Divergent” – Move towards each other “Convergent” – Slide past each other “Transform Fault” Plate Tectonics • Divergent • Examples: – Atlantic Ocean Mid-Ocean Ridge – Red Sea – Iceland – African Rift Valley Plate Tectonics Plate Tectonics Plate Tectonics Plate Tectonics • Convergent – Oceaniccontinental – Oceanic-Oceanic – ContinentalContinental Plate Tectonics • Oceanic-Continental – Ocean plate sinks under the continental plate • • • • Subduction Forms a Trench Forms a Continental Volcanic Arc Earthquakes – Examples: • West coast of the United States and South America Plate Tectonics • Oceanic-Oceanic – One Ocean plate sinks under the other • • • • Subduction Forms a Trench Forms a Volcanic Island Arc Earthquakes – Examples: • Japan • Caribbean Islands Plate Tectonics • Continental-Continental – Continent crashes into Continent • No subduction after Continents hit. • Forms Mountains • Earthquakes – Examples: • Himalayas • Appalachia • Urals Plate Tectonics • Transform Fault – One plate grinds past another • Deforms the surface • Earthquakes – Examples: • San Andreas Fault • Anatolian Fault – Turkey • Chaman Fault - Pakistan Plate Tectonics • Evidence for Plate Tectonics – Paleomagnetism • The natural remnant magnetism in rock bodies • When rock solidifies from the molten state the magnetic crystals that form align with the magnetic field of the earth. • The Earths magnetic field has flipped many times in the past. • This shows up as alternating strips of polarity in the rocks of the seafloor. Plate Tectonics • Evidence for Plate Tectonics – Earthquake patterns • Most earthquakes happen along plate boundaries and happen at different depths according to the type of boundary. – Ocean Drilling • Data on age of seafloor crust supports seafloor spreading. – Hot Spots • Hawaiian Island chain supports the idea that the plates are moving. Plate Tectonics • Mechanisms of Plate Tectonics – Slab-Pull and Ridge-Push • Slab-Pull – As the slab sinks down into the mantle it pulls the rest of the plate after it. • Ridge-Push – The push of the magma from the mantle at the ridge causes the material at the top of the ridge to fall down the sides of the ridge. – Mantle Convection • Currents of rock moving in the earths interior over millions of years. – Cool rock sinking – Hot rock rising