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Rayleigh wave

American  

noun

Mechanics, Geology.
  1. a wave along the surface of a solid, elastic body, especially along the surface of the earth.


Rayleigh wave Scientific  
  1. A type of seismic surface wave that moves with a rolling motion that consists of a combination of particle motion perpendicular and parallel to the main direction of wave propagation. The amplitude of this motion decreases with depth. Like primary waves, Rayleigh waves are alternatingly compressional and extensional (they cause changes in the volume of the rocks they pass through). Rayleigh waves travel slower than Love waves.


Etymology

Origin of Rayleigh wave

First recorded in 1915–20; named after J. W. S. Rayleigh

Example Sentences

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Ritsema, J., Deuss, A., van Heijst, H. J. & Woodhouse, J. H. S40RTS: a degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal-mode splitting function measurements.

From Nature