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This demonstration elucidates the concept of propagation of compressional waves (primary or P waves) and shear waves (secondary or S waves), which constitute the seismic waves used in locating and modeling earthquakes and underground nuclear explosions, and for imaging the interior structure of the Earth. The demonstration uses a slinky, pushed along its axis to create a compressional (longitudinal) wave, and moved up and down on one end to create a shear (transverse) wave.
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Intended for grade levels:
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Technical requirements:
No specific technical requirements, just a browser required
Cost / Copyright:
No cost
Copyright and Other Restrictions Information is Unknown
DLESE Catalog ID:
DLESE-000-000-006-227
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Educational standards:
Resource contact / Creator / Publisher:
Author:
Jeffrey S. Barker Geological Sciences and Environmental Studies, Binghamton University |