1 / 25

Earthquakes

Earthquakes. Today’s Journey.  0507.7.1 Create a model to illustrate geologic events responsible for changes in the earth’s crust.  0507.7.2 Prepare a chart to compare how volcanoes, earthquakes, faulting, and plate movements affect the earth’s surface features.

jewell
Download Presentation

Earthquakes

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Earthquakes

  2. Today’s Journey • 0507.7.1 Create a model to illustrate geologic events responsible for changes in the earth’s crust. • 0507.7.2 Prepare a chart to compare how volcanoes, earthquakes, faulting, and plate movementsaffect the earth’s surface features. • State Performance Indicators • SPI 0507.7.1 Describe internal forces such as volcanoes, earthquakes, faulting, and plate movements thatare responsible for the earth’s major geological features such as mountains, valleys, etc.

  3. 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 (Transform Boundaries) • Caused by volcanic or magmatic activity, • Caused by other sudden stress changes in the earth.

  4. Three Types of Faults Strike-Slip Thrust Normal

  5. What causes earthquakes? • Tectonic plates move past each other causing stress-built up energy on a fault. Stress causes the rock to deform. • The amount of energy released depends on how much rock breaks and how far the blocks of rock move.

  6. Focus – point inside the Earth where an earthquake begins; most of these are less than 45 mi below the surface. Epicenter – point on Earth’s surface above focusWhere do you think would the intensity be strongest?

  7. The hardest shaking is going to be at the epicenter of an earthquake because the seismic waves at the focus of an earthquake are the strongest and the epicenter is directly above it. • These seismic waves spread out from the focus. As they do, their energy grows weaker.

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

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

  10. There are two types of Seismic Waves • Body Waves-move through the “body” of the Earth or the inside. • They can pass through rock and liquid. • Surface waves-move along Earth’s surface.

  11. Primary Waves (P Waves) • A type of seismic body wave that compresses and expands the ground • The first wave to arrive at an earthquake • When they reach the surface, they cause rock to move back and forth. http://daphne.meccahosting.com/~a0000e89/insideearth2.htm

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

  13. Comparing Seismic WavesMake a quick venn diagram to compare the two types of body waves that occur due to an earthquake.

  14. Surface Waves • Move along the Earth’s surface • Known as L waves • 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 because they make the ground swell and roll like ocean waves. • Do not travel too far from the epicenter.

  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 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 6: Very Strong 7: Severe 2-4: Moderate- Weak 8: Violent 9: Extreme 5: Strong

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

  21. Earthquake Waves & Earth’s Interior Bill Nye Earthquake Clip

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

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

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

  25. Today’s Journey • 0507.7.1 Create a model to illustrate geologic events responsible for changes in the earth’s crust. • 0507.7.2 Prepare a chart to compare how volcanoes, earthquakes, faulting, and plate movementsaffect the earth’s surface features. • State Performance Indicators • SPI 0507.7.1 Describe internal forces such as volcanoes, earthquakes, faulting, and plate movements thatare responsible for the earth’s major geological features such as mountains, valleys, etc.

More Related