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  1. Seismology is the scientific study of earthquakes and the propagation of waves through the Earth or through other planet-like bodies. The field also includes studies of earthquake effects, such as tsunamis as well as diverse seismic sources such as volcanic, tectonic, oceanic, atmospheric, and artificial processes (such as explosions).
    en.wikiversity.org/wiki/Seismology
    Seismology is the study of what is under the surface of the Earth by measuring vibrations on the Earth's surface. A person who does this is called a seismologist. It is part of the science of geophysics, which studies the physics of the processes that formed the Earth and other planets.
    simple.wikipedia.org/wiki/Seismology
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    Seismology ( / saɪzˈmɒlədʒi, saɪs -/; from Ancient Greek σεισμός ( seismós) meaning "earthquake" and -λογία ( -logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through the Earth or other planetary bodies.
    en.wikipedia.org
    This field includes the study of other phenomena related to earthquakes like volcanic, tectonic, oceanic, atmospheric processes. Seismology is the study of earthquakes and the propagation of elastic waves through planets and other solid bodies.
    seismology, scientific discipline that is concerned with the study of earthquakes and of the propagation of seismic waves within the Earth. A branch of geophysics, it has provided much information about the composition and state of the planet’s interior.
    Seismic waves are studied by seismologists, who record the waves using seismometers, hydrophones (in water), or accelerometers. Seismic waves are distinguished from seismic noise (ambient vibration), which is persistent low-amplitude vibration arising from a variety of natural and anthropogenic sources.
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    Seismology is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through the Earth or other planetary bodies. It also includes studies of earthquake environmental effects such as tsunamis as well as diverse seismic sources such as volcanic, … See more

    Scholarly interest in earthquakes can be traced back to antiquity. Early speculations on the natural causes of earthquakes were included in the … See more

    Seismic waves are elastic waves that propagate in solid or fluid materials. They can be divided into body waves that travel through the interior … See more

    Seismic waves produced by explosions or vibrating controlled sources are one of the primary methods of underground exploration in … See more

    Because seismic waves commonly propagate efficiently as they interact with the internal structure of the Earth, they provide high-resolution noninvasive methods for studying the planet's interior. One of the earliest important discoveries (suggested by See more

    Detection of seismic waves image

    One of the first attempts at the scientific study of earthquakes followed the 1755 Lisbon earthquake. Other notable earthquakes that … See more

    Seismometers are sensors that detect and record the motion of the Earth arising from elastic waves. Seismometers may be deployed at the … See more

    Earthquake prediction
    Forecasting a probable timing, location, magnitude and other important features of a forthcoming seismic event is called earthquake prediction. … See more

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  4. WebReflection seismology (or seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth's subsurface from reflected seismic waves. The …

  5. WebSeismology's rich history begins with Robert Hooke's 1676 paper titled "True Theory of Elasticity or Springness" and continues through the 1830 discovery of P and S waves, the 1930's discovery of the inner core by …