Seismic Wave Dynamics
Understanding seismic waves reveals the complexities of how they travel through the Earth. Love waves, with their side-to-side motion, are particularly destructive as they can tear structures apart, while Rayleigh waves mimic the rolling motion of ocean waves and can also cause damage, albeit typically less severe. The sequence of wave detection follows a clear pattern: first the p waves, then s waves, and finally the slower surface waves.In this clip
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The Science of Everything Podcast
Episode 125: Earthquakes
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