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Plate Tectonics Current Theory
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Plate Tectonics Theory that explains how large pieces of the lithosphere (Plates) move and change shape (Holt 247). Driving force is convection current in the mantle
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Evidences
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Mid-Ocean Ridges Long undersea mountain chain with narrow valleys and step sides. Form by “…magma rises from the asthenosphere, and that creates new oceanic lithosphere as tectonic plates move apart” (Holt 242). Found most earthquakes happened at these ridges
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Seafloor Spreading Harry Hess and Robert Dietz (1960s) Crust separates at mid-ocean ridges New seafloor forms from upwelling of magma into cracks Seafloor spreads as new magma is brought out
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Seafloor Spreading Continues J. Tuzo Wilson (1965) Canadian geologist Described his idea as rigid “plates,” three boundary types pricellaea52.edublogs.org
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Paleomagnetism The recording of the magnetic field in ancient rocks that gives the direction and intensity of Earth’s magnetic poles at the time the rocks formed. Provided evidence for seafloor spreading Pattern was symmetric around the ocean ridges
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Geological Earthquakes and volcanoes Most are found along plate boundaries http://earthquake.usgs.gov/earthquakes/re centeqsww/ http://earthquake.usgs.gov/earthquakes/re centeqsww/ http://www.iris.edu/seismon/bigmap/index. phtml http://www.iris.edu/seismon/bigmap/index. phtml http://earthquake.usgs.gov/earthquakes/re centeqsus/Maps/US2/40.42.-113.-111.php http://earthquake.usgs.gov/earthquakes/re centeqsus/Maps/US2/40.42.-113.-111.php
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Fossils
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