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Image: Earthquake wave shadow zone

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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.
Author: United States Geological Survey, SVG by Vanessa Ezekowitz
Usage Terms: Creative Commons Attribution-Share Alike 3.0
License: CC-BY-SA-3.0
License Link: http://creativecommons.org/licenses/by-sa/3.0/
Attribution Required?: Yes

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