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Earthquakes! **Adapted from www.middleschoolscience.com
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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 magma activity, Caused by other sudden stress changes in the earth.
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Three Types of Faults Strike-Slip Thrust Normal
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What causes earthquakes? Tectonic plates move past each other causing stress. Stress causes the rock to deform, break, and/or move
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Elastic Rebound – deformed rock goes back to its original shape http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
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Focus – point inside the Earth where an earthquake begins Epicenter – point on Earth’s surface above focus
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How Seismographs Work Normally everything would move, but…. the pendulum remains fixed as the ground moves beneath it …this mass, like the pen, has inertia and so resists motion. It’s a weighted pen writing on a rolling drum of paper.
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Typical Seismogram http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt
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Primary Waves (P Waves) PUSH-PULL PATTERN! – A type of seismic wave that pushes & pulls the ground The FIRST wave to arrive from an earthquake—travels the fastest! Travels Parallel to the direction the wave travels http://daphne.meccahosting.com/~a0000e89/insideearth2.htm
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Secondary Waves (S Waves) A type of seismic wave that moves the ground up and down or side-to-side (perpendicular) to the direction the wave travels Slower! More destructive to buildings http://daphne.meccahosting.com/~a0000e89/insideearth2.htm
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Comparing Seismic Waves **P & S Wave song: http://www.youtube.com/watch?v=w3NLexYxR7ghttp://www.youtube.com/watch?v=w3NLexYxR7g
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Surface Waves Move along the Earth’s surface – ROLL OUT! Motion can be up and down, around & back & forth Travel more slowly than S and P waves – Last to arrive Most destructive to structures
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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 difference between the arrivals of the P waves and the S waves
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Locating Earthquakes Distance (km) Difference in arrival times Question: Where could the EQ be? P-wave S-wave Answer: Anywhere along the blue line. (not much help) 2. Find the distance to the EQ using the lag time and this Time/Distance graph. 3. Use the distance from the EQ as the radius (r) for this circle. r 1.Find the difference in the arrival times, or lag time ( t ), of the P & S waves. Time ( t)
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Locating Earthquakes \ Arrival diff. \ Question: Where could the EQ be, now? Difference in arrival time **Let’s get someone else that has readings for this EQ to help out… (Same procedure) Answer: Where the green and blue circles cross. (Better, but still a 50-50 change of going to the right place to find the EQ.)
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Locating Earthquakes Answer: Where all 3 circles intersect Difference in arrival time \ Arrival diff. \ \ Arrival time diff. \ So, no more guessing– Question: where is the actual EQ ? **If you get 3 people working on this puzzle, now you can triangulate.
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How are Earthquakes Measured? Richter Scale-measures energy
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How are Earthquakes Measured? Mercalli Scale-measures damage 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
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Earthquake Waves & Earth’s Interior **See how seismic waves move through the Earth’s layers here (Shadow zone): http://www.classzone.com/books/earth_science/terc/content/visualizations/es1009/es1009page01.cfm http://www.classzone.com/books/earth_science/terc/content/visualizations/es1009/es1009page01.cfm
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Seismic Waves in the Earth http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
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Tsunamis http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
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Formation of a tsunami http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt
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Tsunami Warning System http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt
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