Earthquakes are basically sound waves seismic waves


Earthquakes are basically sound waves (seismic waves) traveling through the earth. Because the earth is solid, it can support both “P waves” (longitudinal) and “S waves” (transverse). The P waves travel at 8000m/s, while S waves are slower, only 4500 m/s. A seismograph records the two waves from a distant earthquake. If the S wave arrives 2.0 min after the P wave, how far away was the earthquake? 

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Physics: Earthquakes are basically sound waves seismic waves
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