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Geology: Plate Tectonics
By: Ms. Kristin Wilkinson
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Plate Tectonics Pangea Eurasia North America Africa South America
India Australia Plate Tectonics Antarctica
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1-2. Continental Drift (Old Theory)
Alfred Wegener (1900’s) proposed Continents were once a single land mass that drifted apart called- Pangea Evidence or proof! Fossils of the same plants and animals are found on different continents Called this supercontinent Pangea, Greek for “all Earth.” Continents fit like a puzzle 245 Million years ago Split again – Laurasia & Gondwana 180 million years ago
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3. What are Plates? Greek – “tektonikos” of a builder
Pieces of the lithosphere that move around Each plate has a name Fit together like jigsaw puzzles Float on top of mantle similar to ice cubes in a bowl of water
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Tectonic Plates
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4. Evidence for Continental Drift
Fossil Clues Animals Mesosaurus is a reptile found only in S. America & Africa Plant Climate Clues Glacial deposits Rock surfaces Rock Clues A golden orb-weaver spider from the Middle Jurassic Inocaulis Silurian Plant Fossil
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Evidence of Pangea
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5. Theory of Plate Tectonics
Due to the mapping of the ocean floor scientists discovered mid-ocean ridges, thus leading towards this new theory. Seafloor spreading creates new crust along the ridge and older crust is pushed farther away from ridge.
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CONVECTION CURRENT!!! 6. How Do Plates Move?
Tectonics and Volcanism II
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7. Plate Boundaries Divergent Boundaries – plates move AWAY from each other. Convergent Boundaries – plates move TOWARD each other. Transform Boundaries – plates SLIDE past each other.
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Divergent Boundary – Arabian and African Plates
Arabian Plate Red Sea African Plate
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Divergent Boundary – Iceland
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Iceland
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Divergent Boundary - Oceanic
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Divergent Boundary - Continental
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Convergent Boundary – Indian and Eurasian Plates
Indian Plate
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Convergent Boundary – Oceanic & Continental
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Convergent Boundary – Oceanic & Oceanic
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Convergent Boundaries - Continental
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Transform Boundary – San Andreas Fault
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Review Name the 3 main layers of the Earth. What is a tectonic plate?
What was Pangea? Name the three different types of plate boundaries and one location on Earth for each one
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11. Dynamic Earth Forces that Shape Earth
Isostasy – the relationship between crust and asthenosphere Vertical Stress Subsidence and Uplift Horizontal Stress Compression Tension Shearing
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Dynamic Earth… Slow Changes… Rapid Changes to the Earth’s Surface
Earthquakes, Tsunami’s, Volcanic Eruptions Slow Changes… Mountain building, Ridge building, island arcs, Volcanic arcs &hot spots
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12. Landforms Created by Compression
Mountain ranges Ocean trenches Volcanic arcs Island arcs
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13. Landforms Created by Tension
Mid-ocean ridges Continental rifts
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14. Landforms Created by Shearing
Transform Faults
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