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Earthquakes. What is an earthquake? Used to describe the sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by.

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Presentation on theme: "Earthquakes. What is an earthquake? Used to describe the sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by."— Presentation transcript:

1 Earthquakes

2 What is an earthquake? Used to describe the sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip Caused by other sudden stress changes in the earth.

3 Plate Tectonics The Earth’s crust is made of giant plates of rock floating on the liquid mantle (interior of earth) The plates move on the mantle; some places spreading apart, some places coming together, and some places sliding past each other A fault is a line where the plates touch http://www.pbs.org/wgbh/aso/tryit/tectonics/intro.html

4 What causes earthquakes? Tectonic plates move past each other causing stress. Stress causes the rock to deform – Elastic deformation – rock stretches then reaches a breaking point, releasing energy.

5 Elastic Rebound – deformed rock goes back to its original shape http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM

6 Focus – point inside the Earth where an earthquake begins Epicenter – point on Earth’s surface above focus

7 Primary Waves (P Waves) A type of seismic wave that compresses and expands the ground The first wave to arrive at an earthquake http://daphne.meccahosting.com/~a0000e89/insideearth2.htm

8 Secondary Waves (S Waves) A type of seismic wave that moves the ground up and down or side to side http://daphne.meccahosting.com/~a0000e89/insideearth2.htm

9 Comparing Seismic Waves

10 Surface Waves Move along the Earth’s surface Produces motion in the upper crust – Motion can be up and down – Motion can be around – Motion can be back and forth Travel more slowly than S and P waves Most destructive part of an earthquake

11 Typical Seismogram http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt

12 How do scientists calculate how far a location is from the epicenter of an earthquake? Scientists calculate the difference between arrival times of the P waves and S waves The further away an earthquake is, the greater the time between the arrival of the P waves and the S waves

13 Locating Earthquakes http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM

14 Locating Earthquakes http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM

15 Locating Earthquakes http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM

16 How are Earthquakes Measured? Richter Scale

17 How are Earthquakes Measured? Mercalli Intensity Scale Click Link for Interactive Demo http://elearning.niu.edu/simulations/images/S_portfolio/Mercalli/Mercalli_Scale.swf http://elearning.niu.edu/simulations/images/S_portfolio/Mercalli/Mercalli_Scale.swf

18 Earthquake Waves & Earth’s Interior

19 Seismic Waves in the Earth http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM


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