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Published byMaria McLaughlin Modified over 9 years ago
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http://www.youtube.co m/watch?v=hSdlQ8x7 cuk
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The Theory of Continental Drift
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Continental Drift Theory Proposed by Alfred Wegener in 1912 250 million years ago, all of the continents were combined into one super-continent called “Pangaea” The continents gradually drifted apart to where they are today
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Evidence to Support the Theory
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“Puzzle Pieces” Continents look like they could be part of a giant jigsaw puzzle
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Distribution of Fossils Plant and animal fossils found on the coastlines of different continents
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Sequence of Rocks Same rock patterns found in South America, India, Africa, Antarctica and Australia
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Ancient Climates Tropical plant remains (coal deposits) found in Antarctica Glaciation in Africa, South America, India, and Australia during the same time
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Problems With The Theory No mechanism for movement of continents Wind and currents could possibly move fossils Theory was not accepted by scientists
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Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics
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What is Plate Tectonics The Earth’s crust and upper mantle are broken into sections called plates Plates move around on top of the mantle like rafts
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What is the Lithosphere? The crust and part of the upper mantle = lithosphere –100 km thick –Less dense than the material below it so it “floats”
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What is the Asthenoshere? The plastic layer below the lithosphere = asthenosphere The plates of the lithosphere float on the asthenosphere
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2 Types of Plates Ocean plates - plates below the oceans Continental plates - plates below the continents
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Questions... What is the theory of plate tectonics? What is the lithosphere? What is the asthenosphere? What is the connection between the two? What are the two types of plates?
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Plate Boundaries
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Divergent Boundaries Boundary between two plates that are moving apart or rifting RIFTING causes SEAFLOOR SPREADING
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Features of Divergent Boundaries Mid-ocean ridges rift valleys fissure volcanoes
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Convergent Boundaries Boundaries between two plates that are colliding There are 3 types…
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Type 1 Ocean plate colliding with a less dense continental plate Subduction Zone: where the less dense plate slides under the more dense plate VOLCANOES occur at subduction zones
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Andes Mountains, South America
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Type 2 Ocean plate colliding with another ocean plate The less dense plate slides under the more dense plate creating a subduction zone called a TRENCH
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Aleutian Islands, Alaska
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Type 3 A continental plate colliding with another continental plate Have Collision Zones: –a place where folded and thrust faulted mountains form.
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Transform Fault Boundaries Boundary between two plates that are sliding past each other EARTHQUAKES along faults
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San Andreas Fault, CA
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Questions... What are the three types of boundaries? What direction do plates go for each? Which boundary has a subduction zone…what occurs at a subduction zone?
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Causes of Plate Tectonics
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Convection Currents Hot magma in the Earth moves toward the surface, cools, then sinks again. Creates convection currents beneath the plates that cause the plates to move.
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Questions... What causes plates to move? How is a convection current formed?
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