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  2. Seismic noise - Wikipedia

    en.wikipedia.org/wiki/Seismic_noise

    Research on the origin of seismic noise [1] indicates that the low frequency part of the spectrum (below 1 Hz) is principally due to natural causes, chiefly ocean waves.In particular the globally observed peak between 0.1 and 0.3 Hz is clearly associated with the interaction of water waves of nearly equal frequencies but probating in opposing directions.

  3. Rayleigh wave - Wikipedia

    en.wikipedia.org/wiki/Rayleigh_wave

    Rayleigh waves are distinct from other types of surface or guided acoustic waves such as Love waves or Lamb waves, both being types of guided waves supported by a layer, or longitudinal and shear waves, that travel in the bulk. Rayleigh waves have a speed slightly less than shear waves by a factor dependent on the elastic constants of the ...

  4. Reflection seismology - Wikipedia

    en.wikipedia.org/wiki/Reflection_seismology

    A Rayleigh wave typically propagates along a free surface of a solid, but the elastic constants and density of air are very low compared to those of rocks so the surface of the Earth is approximately a free surface. Low velocity, low frequency and high amplitude Rayleigh waves are frequently present on a seismic record and can obscure signal ...

  5. Seismic wave - Wikipedia

    en.wikipedia.org/wiki/Seismic_wave

    Love waves are horizontally polarized shear waves (SH waves), existing only in the presence of a layered medium. [9] They are named after Augustus Edward Hough Love, a British mathematician who created a mathematical model of the waves in 1911. [10] They usually travel slightly faster than Rayleigh waves, about 90% of the S wave velocity.

  6. Surface wave inversion - Wikipedia

    en.wikipedia.org/wiki/Surface_wave_inversion

    Surface waves are classified into two basic types, Rayleigh waves and Love waves. Rayleigh waves travel in a longitudinal manner (the wave motion is parallel to the direction of wave propagation) with particle motion in a retrograde elliptical motion (Figure 1). The Rayleigh waves result from the interaction between P-waves and vertically ...

  7. Seismic magnitude scales - Wikipedia

    en.wikipedia.org/wiki/Seismic_magnitude_scales

    S waves may take an hour to reach a point 1000 km away. Both of these are body-waves, that pass directly through the earth's crust. Following the S waves are various kinds of surface-waves – Love waves and Rayleigh waves – that travel only at the earth's surface. Surface waves are smaller for deep earthquakes, which have less interaction ...

  8. Heavy surf causes coastal chaos across SLO County. See the ...

    www.aol.com/news/heavy-surf-causes-coastal-chaos...

    Waves battered the shores of San Luis Obispo County Thursday morning as high tides washed onto streets, closed piers and parking lots and prompted multiple water rescues up and down the coast.

  9. Surface wave - Wikipedia

    en.wikipedia.org/wiki/Surface_wave

    At this frequency, the silver behaves approximately as a perfect electric conductor, and the SPP is called a Sommerfeld–Zenneck wave, with almost the same wavelength as the free-space wavelength. The surface plasmon polariton (SPP) is an electromagnetic surface wave that can travel along an interface between two media with different ...

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