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Chapter 9 Earthquakes.

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Presentation on theme: "Chapter 9 Earthquakes."— Presentation transcript:

1 Chapter 9 Earthquakes

2 Forces inside Earth Elastic Limit – point at which rocks will remain bent or break, due to applied stresses. Faults – surfaces along which rocks break and move in different directions relative to the fault surface. Earthquake – the movement of the ground, caused by waves from energy released as rocks move along faults.

3 Types of Faults Normal Fault Reverse Fault Strike-Slip Fault
Plates move apart; Tension Plates crash into each other; Compression Rocks move past each other; Shearing Ex. Mid Ocean Ridge Ex. Rocky Mountains Ex. San Andreas Fault Aka Divergent Boundary Aka Convergent Boundary Aka Transform Fault Boundary

4 Earthquake Information
Focus – the point in Earth’s interior where earthquake energy is released. Epicenter – the point on Earth’s surface directly above an earthquake’s focus.

5 Seismic Waves These are the waves of energy that move outward from the earthquake’s focus and make the ground shake Primary Waves – travel through the Earth by causing particles in rocks to compress and stretch apart (back and forth) in the direction of the wave. FASTEST WAVES Secondary Waves - travel through the Earth by causing particles in rocks to move at right angles to the direction of the wave.

6 Primary Waves – travel through the Earth by causing particles in rocks to compress and stretch apart (back and forth) in the direction of the wave. (FASTEST WAVES) Secondary Waves - travel through the Earth by causing particles in rocks to move at right angles to the direction of the wave.

7 Surface Waves These waves are emitted from the epicenter of an earthquake. Give particles an elliptical and back/forth motion. These cause buildings to collapse. These waves cause the most destruction. (SLOWEST WAVES)


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