S-waves
Shear earthquake waves
S-waves are seismic waves that move through rock by shearing it side-to-side, perpendicular to the wave's direction of travel.
Unlike P-waves, which compress and expand material, S-waves cannot pass through liquids or gases—their inability to traverse Earth's outer core helped prove it was molten.
S-waves travel more slowly than P-waves and typically cause more damage during earthquakes.
The S stands for secondary, since they arrive at seismographs after the faster primary waves.
Seismic ground movement
- seismographEarthquake measuring device
- P-wavesLongitudinal seismic vibrations
- body wavesSeismic energy within earth
- transverseExtending sideways across
seismology · epicenter · magnitude · fault · tremor · aftershock · tectonic · Richter scale
Maximum oscillation displacement
- frequencyRate of recurrence
- wavelengthSpatial repetition interval
- oscillationRepeated back-and-forth movement
- perpendicularAt right angles
medium · propagation · energy transfer · waveform · polarization · attenuation · refraction
Break in continuity
- lithosphereCrust plus upper mantle
- asthenosphereDuctile upper mantle layer
- subsurfaceBelow the outer layer
- reflectionReturned light or thought
earthquake
Seismic ground movement
- seismographEarthquake measuring device
- P-wavesLongitudinal seismic vibrations
- body wavesSeismic energy within earth
transverse · seismology · epicenter · magnitude · fault · tremor · aftershock · tectonic · Richter scale · seismometer
amplitude
Maximum oscillation displacement
- frequencyRate of recurrence
- wavelengthSpatial repetition interval
- oscillationRepeated back-and-forth movement
perpendicular · medium · propagation · energy transfer · waveform · polarization · attenuation · refraction
discontinuity
Break in continuity
- lithosphereCrust plus upper mantle
- asthenosphereDuctile upper mantle layer
- subsurfaceBelow the outer layer