Page 4: Research news on seismic wave

A seismic wave is an elastic disturbance that propagates through the Earth or along its surface as a result of sudden stress changes, typically from fault rupture, volcanic activity, or anthropogenic sources such as explosions. Governed by the equations of elastodynamics, seismic waves are categorized into body waves (P and S waves) and surface waves (Rayleigh and Love waves), each with distinct particle motion, dispersion, and attenuation characteristics. Their propagation properties—velocity, amplitude, frequency content, and scattering—are strongly controlled by the elastic moduli, density, anisotropy, and heterogeneity of the medium, making seismic waves a primary observational phenomenon in seismology and Earth structure studies.

Why seismic waves spontaneously race inside the Earth

Earthquakes, volcanic eruptions, shifting tectonic plates—these are all signs that our planet is alive. But what is revealed deep inside Earth surprises laymen and scientists alike: Almost 3000 kilometers below Earth's surface, ...

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