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Topic: What Causes Earthquakes? PSSA: 3.5.7.A / S8.D.1.1
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Objective: TLW explain where earthquakes take place. TLW describe the types of faults associated with plate boundaries. TLW compare the three types of waves that are generated by earthquakes.
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MI #1: Seismology An earthquake is a movement or trembling of the ground caused by a sudden release of energy when rocks move along a fault. Seismology is the study of earthquakes.
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MI #2: Where do earthquakes occur? Most earthquakes occur along tectonic plate boundaries. Faults, or breaks in the Earth’s crust, happen along these boundaries.
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MI #3: What causes earthquakes? Deformation is primarily responsible for causing earthquakes. Plastic deformation is like molded clay and does not cause earthquakes. Elastic deformation occurs when rock under stress is stretched without breaking (like a rubber band). Elastic rebound occurs when elastically deformed rock snaps back to its original shape.
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MI #4: Faults at Plate Boundaries Transform Boundary = Strike-slip fault Convergent Boundary = Reverse Fault Divergent Boundary = Normal Fault
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MI #5: Seismic Waves Seismic waves are waves of energy that travel through the earth away from an earthquake in all directions. Body waves travel through the Earth’s interior, while surface waves travel along Earth’s surface.
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MI #6: Types of Seismic Waves P waves: aka Primary waves, compressional, fastest earthquake waves S waves: aka Secondary waves, side to side motion, second fastest Surface waves: move like water waves, slowest, most destructive
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So What…? Real Life Application Understanding earthquake waves is important to understanding how earthquake epicenters are located.
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