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  2. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    In its most general sense, the word earthquake is used to describe any seismic event that generates seismic waves. Earthquakes can occur naturally or be induced by human activities, such as mining, fracking, and nuclear tests. The initial point of rupture is called the hypocenter or focus, while the ground level directly above it is the epicenter.

  3. Earthquake cycle - Wikipedia

    en.wikipedia.org/wiki/Earthquake_Cycle

    [3] [4] Depending on the size of the earthquake, an earthquake cycle can last decades, centuries, or longer. [ 1 ] [ 5 ] The Parkfield portion of the San Andreas fault is a well-known example where similarly located M6.0 earthquakes have been instrumentally recorded every 30–40 years.

  4. Types of earthquake - Wikipedia

    en.wikipedia.org/wiki/Types_of_earthquake

    Submarine earthquake, an earthquake that occurs underwater at the bottom of a body of water, especially an ocean. [17] Supershear earthquake, an earthquake in which the propagation of the rupture along the fault surface occurs at speeds in excess of the seismic shear wave (S-wave) velocity, causing an effect analogous to a sonic boom. [18]

  5. Earthquakes happen all the time, you just can't feel them. A ...

    www.aol.com/earthquakes-happen-time-just-cant...

    A major earthquake measuring 7.4 hit Taiwan early Wednesday, killing 9 and injuring at least 1,000. A 7.4 earthquake is exponentially more destructive than the 4.8 quake that struck central New ...

  6. Why did Central Mass. feel the earthquake 200 miles away ...

    www.aol.com/why-did-central-mass-feel-214622768.html

    Mitchell explained the area of Friday’s quake is on an ancient fault line. The Earth’s crust responded to broad stresses, and the area of the epicenter happened to be a weak spot ...

  7. Seismic wave - Wikipedia

    en.wikipedia.org/wiki/Seismic_wave

    Earthquakes create distinct types of waves with different velocities. When recorded by a seismic observatory, their different travel times help scientists locate the quake's hypocenter. In geophysics, the refraction or reflection of seismic waves is used for research into Earth's internal structure. Scientists sometimes generate and measure ...

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

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

    Every year tens of millions of people take part in a massive earthquake drill called the Great ShakeOut, which teaches people what to do and how to respond in case of a ground-rattling temblor.

  9. Seismic communication - Wikipedia

    en.wikipedia.org/wiki/Seismic_communication

    Seismic or vibrational communication is a process of conveying information through mechanical vibrations of the substrate. The substrate may be the earth, a plant stem or leaf, the surface of a body of water, a spider's web, a honeycomb, or any of the myriad types of soil substrates.