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  2. Seismology - Wikipedia

    en.wikipedia.org/wiki/Seismology

    Engineering seismology is the study and application of seismology for engineering purposes. [29] It generally applied to the branch of seismology that deals with the assessment of the seismic hazard of a site or region for the purposes of earthquake engineering. It is, therefore, a link between earth science and civil engineering. [30]

  3. Mohorovičić discontinuity - Wikipedia

    en.wikipedia.org/wiki/Mohorovičić_discontinuity

    The Moho has played a large role in the fields of geology and earth science for well over a century. By observing the Moho's refractive nature and how it affects the speed of P-waves, scientists were able to theorize about the earth's composition. These early studies gave rise to modern seismology. [13]

  4. Hiroo Kanamori - Wikipedia

    en.wikipedia.org/wiki/Hiroo_Kanamori

    Kanamori and American seismologist Thomas C. Hanks developed the moment magnitude scale which replaced the Richter scale as a measurement of the relative strength of earthquakes. [1] [2] [3] Kanamori invented the method for calculating slip distribution on the fault plane by teleseismic waveform with Masayuki Kikuchi. In addition, they studied ...

  5. Earth's inner core - Wikipedia

    en.wikipedia.org/wiki/Earth's_inner_core

    Earth was discovered to have a solid inner core distinct from its molten Earth's outer core in 1936, by the Danish seismologist Inge Lehmann's [7] [8] study of seismograms from earthquakes in New Zealand, detected by sensitive seismographs on the Earth's surface. She deduced that the seismic waves reflect off the boundary of the inner core and ...

  6. Earthquake prediction - Wikipedia

    en.wikipedia.org/wiki/Earthquake_prediction

    Earthquake prediction is a branch of the science of seismology concerned with the specification of the time, location, and magnitude of future earthquakes within stated limits, [1] [a] and particularly "the determination of parameters for the next strong earthquake to occur in a region". [2]

  7. P wave - Wikipedia

    en.wikipedia.org/wiki/P_wave

    In typical situations in the interior of the Earth, the density ρ usually varies much less than K or μ, so the velocity is mostly "controlled" by these two parameters. The elastic moduli P wave modulus , M {\displaystyle M} , is defined so that M = K + 4 3 μ {\textstyle \,M=K+{\tfrac {4}{3}}\mu \,} and thereby v p = M ρ {\displaystyle v ...

  8. Regulators are investigating reports of property damage from ...

    www.aol.com/regulators-investigating-reports...

    But Dr. Benjamin Fernando, a postdoctoral fellow in the department of Earth and planetary sciences at Johns Hopkins who studies seismology, told CNN that it’s also possible that loud sonic booms ...

  9. Seismometer - Wikipedia

    en.wikipedia.org/wiki/Seismometer

    As the earth started to move, the heavy mass of the pendulum had the inertia to stay still within the frame. The result is that the stylus scratched a pattern corresponding with the Earth's movement. This type of strong-motion seismometer recorded upon a smoked glass (glass with carbon soot). While not sensitive enough to detect distant ...