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Earthquakes

Learn about earthquakes and how they occur, the structure of the Earth's crust, seismic waves, locating an epicenter, measuring seismic waves, the Richter scale, earthquake damage, past earthquakes, quake-resistant structures, and tsunamis.

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Earthquakes

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  1. Earthquakes LT – students can describe how the energy of an earthquake travels through the Earth

  2. Earthquakes • Shakings and tremblings that results from the movement of rock beneath the Earth’s surface • Most too small to notice • Earthquakes cause the Earth to shake for less than a minute but can do major damage. NSF North Mississippi GK-8

  3. Is the Earth’s Crust One Solid Sheet? • The crust of Earth is actually broken into plates that fit together like puzzle pieces. NSF North Mississippi GK-8

  4. Who’s Fault is it? • The space between two plates is called a fault. • Because earthquakes occur when two plates rub together, they are often said to occur on fault lines. NSF North Mississippi GK-8

  5. Epicenter The Center of it All • Epicenter – point on surface directly above focus • Where is the epicenter in this picture? NSF North Mississippi GK-8

  6. Seismic Waves • The waves of shaking are called seismic waves. NSF North Mississippi GK-8

  7. Locating an Epicenter • When earthquakes occur, different types of seismic waves are produced. • Different seismic waves travel through Earth at different speeds.

  8. Primary Waves • Primary waves are the fastest, secondary waves are slower • Primary waves(P-waves) cause particles in rocks to move back and forth in the same direction that the wave is traveling.

  9. Secondary Waves • Secondary waves(S-waves) move through Earth by causing particles in rocks to move at right angles to the direction of wave travel. https://youtu.be/Z7eABGpOHv8

  10. Measuring Seismic Waves • Seismographs consist of a rotating drum of paper and a pendulum with an attached pen • When seismic waves reach the seismograph, the drum vibrates but the pendulum remains at rest

  11. Seismograph Stations • Primary waves arrive first at seismograph stations, and secondary waves, which travel slower, arrive second.

  12. Seismograph Stations • This difference in arrival times is used to calculate the distance from the seismograph station to the earthquake epicenter.

  13. Seismograph Stations • If seismic waves reach three or more seismograph stations, the location of theepicenter can be determined. • To locate an epicenter, scientists draw circles around each station on a map.

  14. Seismograph Stations • The radius of each circle equals that station’s distance from the earthquake epicenter. • The point where all three circles intersect is the location of the earthquake epicenter.

  15. The Richter Scale • The Richter scale is used to measure how much shaking an earthquake causes. • The Richter scale gives each earthquake a number from 1-10. • Less than 2 – cannot be felt • 2 and 4 – can be felt but do not cause damage • 5 and 6 – can cause damage • 7-10 are major earthquakes and cause severe damage NSF North Mississippi GK-8

  16. Earthquake Damage NSF North Mississippi GK-8

  17. Past Earthquakes • Most of the earthquakes you hear about are large ones that cause great damage. • However, of all the earthquakes detected throughout the world each year, most have magnitudes too low to be felt by humans. • Scientists record thousands of earthquakes every day with magnitudes of less than 3.0.

  18. Quake Resistant Structures • In older buildings, workers often install steel rods to reinforce building walls. • Such measures protect buildings in areas that are likely to experience earthquakes. • Earthquake Resistant Tower • https://youtu.be/0tFWn_e71qc

  19. Tsunamis • Ocean waves caused by earthquakes are called seismic sea waves, or tsunamis. • Far from shore, a wave caused by an earthquake is so long that a large ship might ride over it without anyone noticing. • https://youtu.be/zxm050h0k2I • Https://youtu.be/p4LFu91Xrw0

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