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  2. S wave - Wikipedia

    en.wikipedia.org/wiki/S_wave

    Unlike P waves, S waves cannot travel through the molten outer core of the Earth, and this causes a shadow zone for S waves opposite to their origin. They can still propagate through the solid inner core: when a P wave strikes the boundary of molten and solid cores at an oblique angle, S waves will form and propagate in the solid medium. When ...

  3. Seismic wave - Wikipedia

    en.wikipedia.org/wiki/Seismic_wave

    P wave and S wave from seismograph Velocity of seismic waves in Earth versus depth. [1] The negligible S-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the S-wave velocity is non-zero. A seismic wave is a mechanical wave of acoustic energy that travels through the Earth or another planetary body.

  4. Low-velocity zone - Wikipedia

    en.wikipedia.org/wiki/Low-velocity_zone

    The LVZ shows a reduction in velocity of about 3–6% with the effect being more pronounced with S-waves compared to P-waves. [9] As is evident from the figure, the reduction and depth over which reduction occurs varies with the choice of tectonic province, that is, regions differ in their seismic characteristics.

  5. Shadow zone - Wikipedia

    en.wikipedia.org/wiki/Shadow_zone

    S wave velocity is equal to: / S wave velocity is entirely dependent on the rigidity of the material it travels through. Liquids have zero rigidity, making the S wave velocity zero when traveling through a liquid. Overall, S waves are shear waves, and shear stress is a type of deformation that cannot occur in a liquid.

  6. Seismic velocity structure - Wikipedia

    en.wikipedia.org/wiki/Seismic_Velocity_Structure

    Deeper into the lower mantle, the debate over seismic characteristics continues, with theories of partial melting around the 1000 km depth mark to justify the attenuation of S-wave velocities. [ 21 ] [ 57 ] This molten state may cause a segregation of materials, resulting in a concentration of magnesium-rich olivine in the lower regions and ...

  7. Transverse wave - Wikipedia

    en.wikipedia.org/wiki/Transverse_wave

    In seismology, shear waves are also called secondary waves or S-waves. Transverse waves are contrasted with longitudinal waves , where the oscillations occur in the direction of the wave. The standard example of a longitudinal wave is a sound wave or "pressure wave" in gases, liquids, or solids, whose oscillations cause compression and ...

  8. Your next great bottle of wine might come from this under-the ...

    www.aol.com/news/next-great-bottle-wine-might...

    The mountains boast geological characteristics that enhance the region’s capacity for producing exceptional grapes. The most prominent of its features is the San Andreas fault, which snakes its ...

  9. Surface wave - Wikipedia

    en.wikipedia.org/wiki/Surface_wave

    Surface waves span a wide frequency range, and the period of waves that are most damaging is usually 10 seconds or longer. Surface waves can travel around the globe many times from the largest earthquakes. Surface waves are caused when P waves and S waves come to the surface. Examples are the waves at the surface of water and air (ocean surface ...