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School Seismology Dave Waltham Department of Earth Sciences Royal Holloway University of London
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Japan, March 11, 2011
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RHUL Recording
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P-waves, S-Waves & Mexican Waves
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Surface Waves
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RHUL Recording PSSurface Waves ~10 mins 05:56:37
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86.03 10:10. Hence, earthquake at 05:56:37 – 00:10:10 = 05:46:27
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Epicentral Distance RHUL 86.03 Japan
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www.bgs.ac.uk/schoolSeismology
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With Plate Boundaries
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Texas Epicentral Distance=90°
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Conclusions Off-shore Japan Occurred at 05:46:27 Large!
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www.usgs.gov
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Large Foreshock Wednesday 9/3/11 Friday 11/3/11
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Aftershocks
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Earthquake Seismology RHUL’s Seismometer Greece 14 Feb 2008 Magnitude 6.7 With aftershock China 12 May 2008 Magnitude 7.9 87 652 fatalities Herefordshire 26 Oct 2008 Magnitude 3.6
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Frequencies 1 Hz 0.1 Hz
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Conclusions School equipment can be used to detect and characterize distant earthquakes. We don’t know how to predict earthquakes. Can the next generation of scientists find a way? Until then, rigorous building codes save lives.
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