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  1. en.wikipedia.org › wiki › Shock_waveShock wave - Wikipedia

    In physics, a shock wave (also spelled shockwave ), or shock, is a type of propagating disturbance that moves faster than the local speed of sound in the medium. Like an ordinary wave, a shock wave carries energy and can propagate through a medium but is characterized by an abrupt, nearly discontinuous, change in pressure, temperature, and ...

  2. Shock is a transient physical excitation. Shock describes matter subject to extreme rates of force with respect to time. Shock is a vector that has units of an acceleration (rate of change of velocity). The unit g (or g) represents multiples of the standard acceleration of gravity and is conventionally used.

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  4. A Shock Response Spectrum (SRS) is a graphical representation of a shock, or any other transient acceleration input, in terms of how a Single Degree Of Freedom (SDOF) system (like a mass on a spring) would respond to that input.

  5. en.wikipedia.org › wiki › ForeshockForeshock - Wikipedia

    Foreshock activity has been detected for about 40% of all moderate to large earthquakes, and about 70% for events of M>7.0. They occur from a matter of minutes to days or even longer before the main shock; for example, the 2002 Sumatra earthquake is regarded as a foreshock of the 2004 Indian Ocean earthquake with a delay of more than two years between the two events.

    Foreshock Date(delay)
    Magnitude(foreshock)
    Location
    Date
    March 5, 2021 (2 hours)
    7.4 Mw
    Kermadec Islands, New Zealand
    March 5, 2021
    December 28, 2020 (1 day)
    5.2 Mw
    December 29, 2020
    July 4, 2019 (1 day)
    6.4 Mw
    California, United States
    July 5, 2019
    April 22, 2017 (2 days)
    4.8 Mw
    Valparaíso Region, Chile
    April 24, 2017
  6. en.wikipedia.org › wiki › AftershockAftershock - Wikipedia

    In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according ...

  7. The scale was calibrated by defining a magnitude 0 shock as one that produces (at a distance of 100 km (62 mi)) a maximum amplitude of 1 micron (1 μm, or 0.001 millimeters) on a seismogram recorded by a Wood-Anderson torsion seismometer.

  8. Stevens' power law is an empirical relationship in psychophysics between an increased intensity or strength in a physical stimulus and the perceived magnitude increase in the sensation created by the stimulus. It is often considered to supersede the Weber–Fechner law, which is based on a logarithmic relationship between stimulus and sensation, because the power law describes a wider range of ...