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8.2 Measuring Earthquakes A) Seismographs - instruments that record earthquake waves. B) Seismograms electronically recorded ground motion made by seismographs. I. Instruments
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Seismograph
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Seismogram
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II. Earthquake Waves 8.2 Measuring Earthquakes A) Body Waves 1) P waves - Have the greatest velocity of all -Are push-pull waves that push (compress) and pull (expand) - Travel through solids, liquids, and gases
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Earthquake Waves 8.2 Measuring Earthquakes S waves - Slower velocity than P waves - Travel only through solids
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8.2 Measuring Earthquakes Surface waves seismic waves, travel along Earth’s outer layer.
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Seismic Waves
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Locating an Earthquake 8.2 Measuring Earthquakes Earthquake Distance Travel-time graphs from 3 or more seismographs can be used to find the exact location of an earthquake epicenter. The epicenter is located using the difference in the arrival times between P and S wave Earthquake Direction
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Measuring Earthquakes 8.2 Measuring Earthquakes Richter Scale Richter Scale Based on the amplitude of the largest seismic wave. Increases 32 times each increase
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Measuring Earthquakes 8.2 Measuring Earthquakes Moment Magnitude Moment magnitude is the most widely used - estimates the energy released by earthquakes.
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Earthquake Magnitudes
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- The majority of all earthquakes that occur on Earth are found at or near plate boundaries. 8.2 Earthquake locations
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Some Notable Earthquakes
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