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Summary
| Description |
English: Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones. |
| Date | |
| Source | https://pressbooks.bccampus.ca/physicalgeologyh5p/chapter/3-2-understanding-earth-through-seismology-2/ |
| Author | Karla Panchuk, Steven Earle |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 12:37, 2 February 2023 | | 1,496 × 915 (750 KB) | LukeTriton | Uploaded a work by Karla Panchuk, Steven Earle from https://pressbooks.bccampus.ca/physicalgeologyh5p/chapter/3-2-understanding-earth-through-seismology-2/ with UploadWizard |
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