Earthquake Dynamics
Fault rupture occurs when tectonic plates slide past each other, releasing built-up stress as seismic waves. While the classical elastic rebound theory explains much about earthquakes, recent evidence suggests that many faults may be weaker than previously thought, allowing for more gradual deformation before failure. This evolving understanding challenges traditional views and highlights the complexity of seismic activity.In this clip
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The Science of Everything Podcast
Episode 125: Earthquakes
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