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.

In seconds, fiber optic cables detect earthquake size

Scientists have discovered a new way to determine how big an earthquake may become just seconds after it begins. In a new study published in Nature Communications, researchers from the U.S. Geological Survey (USGS) and Cal ...

Every time Norway scores, the whole city of Bergen shakes

During Norway's first match of the FIFA World Cup against Iraq on June 17, several small vibrations were recorded on the seismometer. A particularly clear signal was observed when Erling Haaland scored.

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