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The Big Crack Up!
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Explain the causes of earthquakes and volcanic eruptions.
LEARNING TARGET 4: Describe plate movements that cause ocean basins, ocean trenches, and mountains to form; Explain the causes of earthquakes and volcanic eruptions.
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EARTH: A GIGANTIC RECYCLING CENTER!
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Plate Tectonics The theory of plate tectonics is based on the evaluation of scientific evidence and observation- The Scientific Method Continental Drift hypothesis Seafloor Spreading hypothesis
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Convergent Divergent Transform
Plate Boundaries Convergent Divergent Transform
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Plate Tectonics Explains the configuration of topographic features of the Earth- mountains, valleys, volcanoes, islands, oceanic trenches, faults
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Tectonic plates Are composed of the lithosphere
Move as a coherent mass May contain oceanic crust and continental crust
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Plate Boundaries Where does the energy come from to move plates?
Where does it go? Topographic features on the Earth’s surface reflects what is happening in the mantle.
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Convergent Plate Boundary
Volcanic arc Oceanic crust subducts under continental crust Melting occurs at about 100 miles down Hot more buoyant material rises
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Volcanic Arc Oceanic and continental crust
Cascade Range, Andes, Alaska Characteristics: large volcanoes; subduction zone; trench; oceanic crust subducts under continental crust
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Convergent Plate Boundary
Convergent Plate Boundary Map and cross-section views of the subduction zone The oceanic Juan de Fuca plate subducts under the continental North American Plate
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Convergent Plate Boundary
Two oceanic crusts Oceanic crust subducts under opposing oceanic crust Oldest oceanic crust subducts
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Island Arc Japan, Indonesia, Philippines, Caribbean, Aleutian Islands
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Convergent Plate Boundary
Earthquakes trace the SUBDUCTING SLAB to about 500 miles or 650 kilometers Gold dots represent earthquake hypocenters
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Sketch a cross-section of a convergent plate boundary that contains an oceanic crust.
Label with the following terms: Subduction zone Trench Area of melting Area of volcanism Arrows indicating direction of plate movement
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Convergent Plate Boundaries
Two continental crusts Neither subduct due to buoyancy of crusts Mountains form
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India collided with Asia about 40 million years ago
Mt. Everest, 29,000 feet
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Divergent Plate Boundary
Two plates move apart Run through ocean basins
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Divergent Plate Boundaries
New crust forms at mid-oceanic ridges. The seafloor spreads out. This is Seafloor Spreading.
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In most locations, mid-ocean ridges are 6,500 feet (1,980 m) or more below the surface of the oceans. In a few places, they reach above sea level and form islands. Iceland (North Atlantic), the Azores (west of Portugal), and Tristan de Cunha (south Atlantic between southern Africa and South America)
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How Does Seafloor Spreading Affect Neighboring Plates?
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East Africa Rift Zone Continental crust is beginning to pull-apart forming a rift valley
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Process of Ocean Basin Formation
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Sketch a cross section of a divergent plate boundary.
Label with the following terms: rift valley; oceanic ridge; oceanic crust; location of melting and volcanism; and arrows indicating direction of plate movement .
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Transform Plate Boundary
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Transform Plate Boundary
The tectonic plates pass by each other Connected to other plate boundaries San Andreas Fault Label the plates, their movement directions, and the San Andreas Fault
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Hot Spots Animation of Formation
Stationary plumes of hot material that initiate at the core/mantle interface Hawaii: the plume is beneath oceanic crust
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Hot Spots
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Hot Spots Yellowstone is associated with a hot spot under continental crust
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Name the landform associated with oceanic crust subducting under continental crust. Oceanic crust?
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