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School Seismology Dave Waltham Department of Earth Sciences Royal Holloway University of London

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School Seismology. Dave Waltham Department of Earth Sciences Royal Holloway University of London. Japan, March 11, 2011. RHUL Recording. P-waves, S-Waves & Mexican Waves. Surface Waves. RHUL Recording. 05:56:37. ~10 mins. P. S. Surface Waves. 86.03. - PowerPoint PPT Presentation

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Page 1: School Seismology

School SeismologyDave WalthamDepartment of Earth SciencesRoyal Holloway University of London

Page 2: School Seismology

Japan, March 11, 2011

Page 3: School Seismology
Page 4: School Seismology

RHUL Recording

Page 5: School Seismology

P-waves, S-Waves & Mexican Waves

Page 6: School Seismology

Surface Waves

Page 7: School Seismology

RHUL Recording

P S Surface Waves

~10 mins

05:56:37

Page 8: School Seismology
Page 9: School Seismology

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

Page 11: School Seismology

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!

Page 15: School Seismology

www.usgs.gov

Page 16: School Seismology

Large Foreshock

Wednesday 9/3/11

Friday 11/3/11

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Aftershocks

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EarthquakeSeismology

RHUL’s Seismometer

Greece14 Feb 2008Magnitude 6.7With aftershock

China12 May 2008Magnitude 7.987 652 fatalities

Herefordshire26 Oct 2008Magnitude 3.6

Page 19: School Seismology

Frequencies1 Hz0.1 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.