earthquakes! **adapted from
TRANSCRIPT
Earthquakes!
**Adapted from www.middleschoolscience.com
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.
Three Types of Faults
Strike-SlipThrust
Normal
What causes earthquakes?• Tectonic plates move past each other causing
stress. Stress causes the rock to deform, break, and/or move
Elastic Rebound – deformed rock goes back to its original shape
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
Focus – point inside the Earth where an earthquake begins
Epicenter – point on Earth’s surface above focus
How Seismographs Work
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
the pendulum remains fixed as the ground moves beneath it
Typical Seismogram
http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt
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
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 destructiveto buildings
http://daphne.meccahosting.com/~a0000e89/insideearth2.htm
Comparing Seismic Waves
**P & S Wave song: http://www.youtube.com/watch?v=w3NLexYxR7g
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
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
Locating Earthquakes
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
Locating Earthquakes
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
Locating Earthquakes
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
How are Earthquakes Measured? Richter Scale-measures energy
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
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
Seismic Waves in the Earth
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
Tsunamis
http://www.uwgb.edu/dutchs/EarthSC-102VisualsIndex.HTM
Formation of a tsunami
http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt
Tsunami Warning System
http://isu.indstate.edu/jspeer/Earth&Sky/EarthCh11.ppt