Seismic Waves Slinky Lab
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Seismic Waves Slinky Lab
Field notes: two kinds of seismic waves
At an earthquake, energy travels away from the source as seismic waves. In a P-wave, particles vibrate back and forth in the same direction the wave travels. This longitudinal motion creates compressions, where particles bunch together, and rarefactions, where they spread apart. P-waves are the fastest seismic waves and can travel through solids and liquids. In an S-wave, particles vibrate at right angles to the wave’s travel direction. This transverse motion can travel through solids, but not liquids. S-waves travel more slowly than P-waves. Seismographs record arriving waves; comparing their arrival times helps scientists locate earthquakes and learn about Earth’s interior.
Decode the wave evidence
Use the field notes and the information in each question to answer each question.
- Particles move at right angles to the wave’s travel.
- Particles move back and forth parallel to the wave’s travel.
- Particles move in circles around their starting points.
- Particles move only in the direction the wave travels.
- P-wave, because the coils move parallel to travel
- S-wave, because the coils move perpendicular to travel
- P-wave, because it cannot move through solids
- S-wave, because it travels faster than a P-wave
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