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SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation primary waves/arrive first at a station compressional particle motion in propagation direction like sound waves P Waves Fig. 4.18

P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

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Page 1: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation

•  primary waves/arrive first at a station •  compressional •  particle motion in propagation direction •  like sound waves

P Waves

Fig. 4.18

Page 2: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation

•  secondary waves/arrive second •  shear waves •  particle motion perpendicular to propagation direction •  like waves on a rope

S Waves

Fig. 4.18

Page 3: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation

P and S Waves are body waves

Image: S. Marshak “Earth, Portrait of a Planet”

Page 4: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation

•  arrive just after body waves •  combination of reflected S waves •  particle motion perpendicular to propagation •  motion decreases exponentially with depth •  like spikes in a wheat field

Surface Waves: Love Waves

Image: S. Marshak “Earth, Portrait of a Planet”

Page 5: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation

•  arrive last •  combination of reflected P and S waves •  retrograde elliptical particle motion •  motion decreases exponentially with depth •  like water waves

Surface Waves: Rayleigh Waves

Fig. 4.18 largest signal most damaging wave

retrograde R. waves

prograde water waves

Page 6: P Waves - University of California, San Diegogabi/sio15/supps/seismic-waves.pdfSIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation! P and S Waves are body waves! Image: S. Marshak

SIO15-10: Lecture 7 EQ Seismology and Hazard Mitigation