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Summary
| Description |
Raypaths of S-waves and P-waves through the Earth's mantle and core, illustrating how P- and S-wave detection reveals planetary interiors. Earthquake shadow zones are the zones where seismic waves do not reach. S-waves do not penetrate the outer core, so they are shadowed everywhere more than 104° away from the epicenter. |
| Source | https://earthquake.usgs.gov/learn/glossary/?termID=170&alpha=S (image link) |
| Author | United States Geological Survey, SVG by Vanessa Ezekowitz |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:21, 8 August 2008 | | 379 × 509 (224 KB) | Vanessaezekowitz | Raypaths of S- and P-waves through the Earth's mantle and core, SVG version based on [http://earthquake.usgs.gov/learning/glossary.php?term=shadow zone this image] from the USGS. SVG by Vanessa Ezekowitz |
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