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Earthquakes Liz LaRosa http://www.middleschoolscience.com 2009
for my 5th grade science class 2009
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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 magmatic activity, Caused by other sudden stress changes in the earth.
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Three Types of Faults Strike-Slip Thrust Normal Three types of faults
Form depending on type of plate motion and complex reaction of earth’s lithospheric blocks Strike-slip Normal Thrust Normal
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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.
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Elastic Rebound – deformed rock goes back to its original shape
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Focus –. point inside the Earth where an
Focus – point inside the Earth where an earthquake begins Epicenter – point on Earth’s surface above focus
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How Seismographs Work the pendulum remains fixed as the ground moves beneath it
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Typical Seismogram
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Primary Waves (P Waves)
A type of seismic wave that compresses and expands the ground The first wave to arrive at an earthquake
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Secondary Waves (S Waves)
A type of seismic wave that moves the ground up and down or side to side
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Comparing Seismic Waves
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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
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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 between the arrival of the P waves and the S waves
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Locating Earthquakes
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Locating Earthquakes
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Locating Earthquakes
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How are Earthquakes Measured? Richter Scale
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How are Earthquakes Measured? Mercalli Intensity Scale
Click Link for Interactive Demo
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Earthquake Waves & Earth’s Interior
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Seismic Waves in the Earth
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Tsunamis
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Formation of a tsunami
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Tsunami Warning System
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