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  2. Elastic-rebound theory - Wikipedia

    en.wikipedia.org/wiki/Elastic-rebound_theory

    In geology, the elastic-rebound theory is an explanation for how energy is released during an earthquake. As the Earth's crust deforms, the rocks which span the opposing sides of a fault are subjected to shear stress .

  3. Earthquake cycle - Wikipedia

    en.wikipedia.org/wiki/Earthquake_Cycle

    After Harry F. Reid proposed the elastic-rebound theory in 1910 based on the surface rupture record from the 1906 San Francisco earthquake, and accumulated geodetic data demonstrated continual stress loading from the plate motion, a theory of the "cyclic" earthquake re-occurrence began to form in the late twentieth century.

  4. Ductility (Earth science) - Wikipedia

    en.wikipedia.org/wiki/Ductility_(Earth_science)

    In addition, when a material is behaving ductilely, it exhibits a linear stress vs strain relationship past the elastic limit. [ 1 ] Ductile deformation is typically characterized by diffuse deformation (i.e. lacking a discrete fault plane ) and on a stress-strain plot is accompanied by steady state sliding at failure, compared to the sharp ...

  5. What causes earthquakes? The science behind why seismic ... - AOL

    www.aol.com/causes-earthquakes-science-behind...

    Multiple notable earthquakes have struck the United States this year, including a powerful quake in California and a historic event on the East Coast earlier in 2024. Strong earthquakes can lead ...

  6. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    Tectonic earthquakes occur anywhere on the earth where there is sufficient stored elastic strain energy ... and magnitude of future earthquakes within stated limits. ...

  7. Earthquake prediction - Wikipedia

    en.wikipedia.org/wiki/Earthquake_prediction

    Earthquake prediction is a branch of the science of ... and magnitude of future earthquakes within stated limits, [1 ... According to the elastic rebound ...

  8. 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.

  9. Earthquake engineering - Wikipedia

    en.wikipedia.org/wiki/Earthquake_engineering

    Earthquake loss estimation is usually defined as a Damage Ratio (DR) which is a ratio of the earthquake damage repair cost to the total value of a building. [62] Probable Maximum Loss ( PML ) is a common term used for earthquake loss estimation, but it lacks a precise definition.