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Earthquakes Liz LaRosa 2009http://www.middleschoolscience.com for my 5 th grade science class 2009.

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Presentation on theme: "Earthquakes Liz LaRosa 2009http://www.middleschoolscience.com for my 5 th grade science class 2009."— Presentation transcript:

1 Earthquakes Liz LaRosa http://www.middleschoolscience.com 2009http://www.middleschoolscience.com for my 5 th grade science class 2009

2 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.

3 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.

4 Map of Tectonic Plates and Volcanoes

5 Three Types of Faults Strike-Slip Reverse Normal

6

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

8 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

9 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

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 More destructive

11 How Seismometers work 1. Detects and records the ground motion 2. A large mass is suspended from a wire. It does not move during an earthquake. (all because of inertia) 3. A pen attached to the mass marks a roll of moving paper.

12 How Seismographs Work http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM the pendulum remains fixed as the ground moves beneath it

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

14 Comparing Seismic Waves

15 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

16 Locating Earthquakes- Triangulating the Epicenter http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM

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

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

19 How are Earthquakes Measured? Richter Scale

20 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

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

22 Formation of a tsunami http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt

23 Tsunami Warning System http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt


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