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  2. Earthquake simulation - Wikipedia

    en.wikipedia.org/wiki/Earthquake_simulation

    Earthquake simulation applies a real or simulated vibrational input to a structure that possesses the essential features of a real seismic event. Earthquake simulations are generally performed to study the effects of earthquakes on man-made engineered structures, or on natural features which may present a hazard during an earthquake.

  3. ShakeAlert - Wikipedia

    en.wikipedia.org/wiki/ShakeAlert

    Initially, ShakeAlert processing centers were capable of detecting earthquakes at an early stage because of three specific algorithms. The first algorithm was ElarmS. [33] Also known as Earthquake Alarm Systems, these signals detect the P wave energy released during an earthquake. This energy, while given off quite early, does not usually cause ...

  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

    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.

  6. P wave - Wikipedia

    en.wikipedia.org/wiki/P_wave

    A P wave (primary wave or pressure wave) is one of the two main types of elastic body waves, called seismic waves in seismology. P waves travel faster than other seismic waves and hence are the first signal from an earthquake to arrive at any affected location or at a seismograph. P waves may be transmitted through gases, liquids, or solids.

  7. Travel-time curve - Wikipedia

    en.wikipedia.org/wiki/Travel-time_curve

    Travel time in seismology means time for the seismic waves to travel from the focus of an earthquake through the crust to a certain seismograph station. [1] Travel-time curve is a graph showing the relationship between the distance from the epicenter to the observation point and the travel time.

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  9. Earthquake shaking table - Wikipedia

    en.wikipedia.org/wiki/Earthquake_shaking_table

    Earthquake shaking tables are essential in model testing contests, where participants evaluate designs developed within specific guidelines against simulated seismic activity. [5] Simple shake tables are also used in architecture and structural engineering primarily for educational purposes, helping students learn how structures respond to ...