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CHAPTER 2 Plate Tectonics and the Ocean Floor (B)
Dr. Dong, El Camino College
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Review Chap 2 (A) Evidences to support continental drift
Evidences to support plate tectonics theory
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Plate Tectonics Theory
Lithospheric plates “float” on the asthenosphere Large scale geologic features occur at plate boundaries Driving force of plate motion: Friction: slab suction Gravity: slab pull
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Figure 2.13b: Plates
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Types of Plate Boundaries
Divergent Convergent Transform Fig. 2.14
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Exe 03-01 List three types of plate boundaries
Describe the main content of plate tectonics
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Divergent Boundary Features
Fig. 2.15 Plates move apart Mid-ocean ridge Rift valley New ocean floor created Shallow earthquakes Iceland is the only country which is located along a mid-ocean ridge
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A new ocean is formed Fig. 2.17
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Iceland is located along the mid-ocean ridge
Fig. 2.16
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Red Sea is expanding Fig 2.16
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Exe. 03-02 Describe how a new ocean is formed
Which country is located over the mid-ocean ridge?
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Three Types of Convergent Plate Boundaries
Fig. 2.20
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Convergent Boundary Features
Plates move toward each other Oceanic crust destroyed Ocean trench Volcanic arc Deep earthquakes
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Types of Convergent Boundaries
Oceanic-continental convergence Ocean plate subducted Continental arc Oceanic trench Deep earthquakes
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Fig. 2.21a,b
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Fig. 2.22
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Exe. 03-03 List types of convergent plate boundaries.
How was the Himalayas mountain formed? Explain how St. Helens volcano was formed?
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Transform boundary features
Offsets oriented perpendicular to mid- ocean ridge Segments of plates slide past each other Offsets permit mid-ocean ridge to move apart at different rates Shallow but strong earthquakes
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transform faults Fig. 2-23
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San Andreas Fault Fig. 2.23
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Exe Explain why earthquakes frequently take place in the California?
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Fig. 2.24
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Applications of plate tectonics model to intraplate features
Fig. 2.25
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Fig. 2.26
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Measuring plate motion by satellites
Fig. 2.30
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Exe Explain how Hawaii chain islands were formed ?
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Paleoceanography Reconstructing paleogeography Continental accretion
Continental material added to edges of continents through plate motion Continental separation or rifting Continents move apart
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Paleo-reconstructions
Fig. 2.31
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Future predictions Future positions of continents and oceans
Assume same direction and rate of plate motions as now
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World map 50 million years from now
Fig. 2.32
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Wilson cycle John Tuzo Wilson Life cycle of ocean basins Formation
Growth Destruction
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Wilson cycle Fig. 2.33
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Exe Describe Ocean floor cycle
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