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  2. Volcano tectonic earthquake - Wikipedia

    en.wikipedia.org/wiki/Volcano_tectonic_earthquake

    A volcano tectonic earthquake or volcano earthquake is caused by the movement of magma beneath the surface of the Earth. [1] The movement results in pressure changes where the rock around the magma has a change in stress. At some point, this stress can cause the rock to break or move. This seismic activity is used by scientists to monitor ...

  3. Geophysical global cooling - Wikipedia

    en.wikipedia.org/wiki/Geophysical_global_cooling

    A relationship between earthquakes and volcanoes had been noted, although the causes were not known. Fault lines and earthquakes tended to happen along the boundaries of the shifting "boiler plates", but the folding of mountains indicated that sometimes the plates buckled. [2]

  4. Volcano tectonics - Wikipedia

    en.wikipedia.org/wiki/Volcano_tectonics

    The latter may be directly accessible in the eroded portions of active volcanoes or, more commonly, in extinct eroded volcanoes. The general aim of Volcano-Tectonics is to capture the shallower and deeper structure of volcanoes, establishing the overall stress-strain relationships between the magma and the host rock, to ultimately understand ...

  5. Tectonics - Wikipedia

    en.wikipedia.org/wiki/Tectonics

    Seismotectonics is the study of the relationship between earthquakes, active tectonics, and individual faults in a region. It seeks to understand which faults are responsible for seismic activity in an area by analysing a combination of regional tectonics, recent instrumentally recorded events, accounts of historical earthquakes, and ...

  6. Earth science - Wikipedia

    en.wikipedia.org/wiki/Earth_science

    Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of physical and chemical processes in the Earth's crust. [6] Beneath the Earth's crust lies the mantle which is heated by the radioactive decay of heavy elements.

  7. Seismic velocity structure - Wikipedia

    en.wikipedia.org/wiki/Seismic_Velocity_Structure

    The study of seismic velocity structure, using the principles of seismic wave propagation, offers critical insights into the Earth's internal structure, material composition, and physical states. [1] Variations in wave speed, influenced by differences in material density and state (solid, liquid, or gas), alter wave paths through refraction and ...

  8. Earthquakes increase at Hawaii's Kilauea Volcano as ...

    www.aol.com/earthquakes-increase-hawaiis-kilauea...

    Mount Kilauea, the most active volcano in Hawaii, has seen the number of earthquakes at its summit double over the past week, according to the U.S. Geological Survey.. The summit region had gone ...

  9. Deformation (volcanology) - Wikipedia

    en.wikipedia.org/wiki/Deformation_(volcanology)

    Volcanic earthquakes, or volcanic-tectonic earthquakes, can be caused by the movement of magma or other volcanic fluids, inducing tectonic stress that leads to earthquakes of high frequency. Lower frequency volcanic earthquakes, a result of resonation (physical oscillation from seismic waves) in cracks due to magma movement, may also be ...