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How Do We Know Where an Earthquake Originated?
Jeffrey Barker (Binghamton University) & Michael Hubenthal (IRIS)
Students use real seismograms to determine the arrival times for P and S waves and use these times to determine the distance of the seismic station from the earthquake. Seismograms from three stations are provided to determine the epicenter using the S – P (S minus P) method. Because real seismograms contain some "noise" with resultant uncertainty in locating arrival times of P and S waves, this activity promotes appreciation for uncertainties in interpretation of real scientific data.

Resource Type: Activities:Lab Activity, Classroom Activity
Grade Level: College Lower (13-14), Middle (6-8), High School (9-12)
Subject: Geoscience, Natural Hazards:Earthquakes, Seismology
Special Interest: Process of Science, Quantitative, Data, models, or simulations, Hazards
Quantitative Skills: Estimation, Arithmetic/Computation
On the Cutting Edge Exemplary Collection This activity is part of the On the Cutting Edge Exemplary Teaching Activities collection.
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