Today in class we took a break from building our towers, and instead learned how to read seismograms! We first learned how to identify the arrival of p-waves, s-waves and surface waves on a seismogram. The p-waves always arrived first, and were the smallest, and then the s-waves arrived, and lastlythe surface waves (which were the largest). We then learned how to use the difference in the arrival times of the P and S waves to determine how far away from the epicenter of the earthquake the seismograph was. With using a graph depicting the amount of time it took for the s or p wave to travel a certain distance we were able to apply the time delay between the two waves to discover the seimograph's distance from the epicenter. We recieved a white packet called "reading seismograms" in class today so if you were absent make sure to pick one up.
Wednesday, December 9, 2009
Scribe, Wednesday December 9th
Today in class we took a break from building our towers, and instead learned how to read seismograms! We first learned how to identify the arrival of p-waves, s-waves and surface waves on a seismogram. The p-waves always arrived first, and were the smallest, and then the s-waves arrived, and lastlythe surface waves (which were the largest). We then learned how to use the difference in the arrival times of the P and S waves to determine how far away from the epicenter of the earthquake the seismograph was. With using a graph depicting the amount of time it took for the s or p wave to travel a certain distance we were able to apply the time delay between the two waves to discover the seimograph's distance from the epicenter. We recieved a white packet called "reading seismograms" in class today so if you were absent make sure to pick one up.
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