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Earthquakes

Date post: 12-Jan-2016
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Earthquakes. What is an earthquake?. Used to describe both sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip Caused by volcanic or magmatic activity, Caused by other sudden stress changes in the earth. Three Types of Faults. Strike-Slip. - PowerPoint PPT Presentation
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Page 1: Earthquakes

Earthquakes

Page 2: Earthquakes

What is an earthquake?

• Used to describe both sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip

• Caused by volcanic or magmatic activity, • Caused by other sudden stress changes in the

earth.

Page 3: Earthquakes

Three Types of Faults

Strike-SlipThrust

Normal

Page 4: Earthquakes

What causes earthquakes?• Tectonic plates move past each other causing

stress. Stress causes the rock to deform– Plastic deformation – does not cause earthquakes– Elastic deformation – rock stretches then reaches

a breaking point, releasing energy.

Page 5: Earthquakes

Elastic Rebound – deformed rock goes back to its original shape

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

Page 6: Earthquakes

Focus – point inside the Earth where an earthquake begins

Epicenter – point on Earth’s surface above focus

Page 7: Earthquakes

How Seismographs Work

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

the pendulum remains fixed as the ground moves beneath it

Page 8: Earthquakes

Typical Seismogram

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

Page 9: Earthquakes

Primary Waves (P Waves)

• A type of seismic wave that push and pulls the ground

• The first wave to arrive at an earthquake

http://daphne.meccahosting.com/~a0000e89/insideearth2.htm

Page 10: Earthquakes

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

Page 11: Earthquakes

Comparing Seismic Waves

Page 12: Earthquakes

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• More destructive

Page 13: Earthquakes

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

Page 14: Earthquakes

Locating Earthquakes

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

Page 15: Earthquakes

Locating Earthquakes

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

Page 16: Earthquakes

Locating Earthquakes

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

Page 17: Earthquakes

How are Earthquakes Measured? Richter Scale

Page 18: Earthquakes

How are Earthquakes Measured? Mercalli Intensity Scale

Click Link for Interactive Demo http://elearning.niu.edu/simulations/images/S_portfolio/Mercalli/Mercalli_Scale.swf

Page 19: Earthquakes

Earthquake Waves & Earth’s Interior

Page 20: Earthquakes

Seismic Waves in the Earth

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

Page 21: Earthquakes

Tsunamis

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

Page 22: Earthquakes

Formation of a tsunami

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

Page 23: Earthquakes

Tsunami Warning System

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


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