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  2. 2023 Greenland landslide - Wikipedia

    en.wikipedia.org/wiki/2023_Greenland_landslide

    The event produced an unprecedented very long period (VLP) seismic event observable on seismic stations worldwide for up to nine days. [6] The wave was caught in a narrow fjord which caused the wave to continue to slosh back and forth off the walls for the entire time, [ 7 ] resulting in a global seismic vibration, picked up all over the world ...

  3. Earthquake early warning system - Wikipedia

    en.wikipedia.org/wiki/Earthquake_early_warning...

    An animation detailing how earthquake warning systems work: When P waves are detected, the readings are analyzed immediately, and, if needed, the warning information is distributed to advanced users and cell phones, radio, television, sirens, and PA systems/fire alarm systems before the arrival of S waves. An earthquake warning system or ...

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

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

    An earthquake is what happens when the seismic energy from plates slipping past each other rattles the planet's surface. Those seismic waves are like ripples on a pond, the USGS said.

  5. Focal mechanism - Wikipedia

    en.wikipedia.org/wiki/Focal_mechanism

    The focal mechanism of an earthquake describes the deformation in the source region that generates the seismic waves. In the case of a fault-related event, it refers to the orientation of the fault plane that slipped, and the slip vector and is also known as a fault-plane solution. Focal mechanisms are derived from a solution of the moment ...

  6. Glacial earthquake - Wikipedia

    en.wikipedia.org/wiki/Glacial_earthquake

    Since glacial earthquakes produce large amplitude and long period waves that deviate from traditional tectonic earthquake activity, glacial earthquakes require different monitoring methods. [1] This is a primary reason why the specific class of glacial earthquakes was not discovered until 2003. [1]

  7. Microseism - Wikipedia

    en.wikipedia.org/wiki/Microseism

    For wave trains with a very small difference in frequency (and thus wavenumbers), this pattern of wave groups may have the same velocity as seismic waves, between 1500 and 3000 m/s, and will excite acoustic-seismic modes that radiate away. Wave groups generated by waves with opposing directions. The blue curve is the sum of the red and black.

  8. Expert debunks myths about what to do during an earthquake - AOL

    www.aol.com/news/2015-10-14-expert-debunks-myths...

    Earthquakes only happen due to friction between two blocks of the Earth's crust that suddenly slips, and sends shaking in all directions. However surface soils and hillsides can settle or slump ...

  9. Tectonic weapon - Wikipedia

    en.wikipedia.org/wiki/Tectonic_weapon

    Roger Clark, lecturer in geophysics at Leeds University said in the journal Nature in 1996, responding to a newspaper report that there had been two secret Soviet programs, "Mercury" and "Volcano", aimed at developing a "tectonic weapon" that could set off earthquakes from great distance by manipulating electromagnetism, said "We don't think it is impossible, or wrong, but past experience ...