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

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

    What causes earthquakes? Earthquakes occur when the plates that make up the Earth's crust move around. These plates, called tectonic plates, can push against each other.

  3. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    Earthquakes can cause fires by damaging electrical power or gas lines. In the event of water mains rupturing and a loss of pressure, it may also become difficult to stop the spread of a fire once it has started. For example, more deaths in the 1906 San Francisco earthquake were caused by fire than by the earthquake itself. [72]

  4. How are earthquakes triggered and how are their magnitudes ...

    www.aol.com/news/earthquakes-triggered...

    Here are some earthquake basics, ... Here are some earthquake basics, like what earthquake magnitudes mean and how much damage each can cause.

  5. Why do earthquakes happen? - AOL

    www.aol.com/causes-earthquake-natural-disaster...

    Movement of tectonic plates against each other sends seismic waves rippling across earth’s surface

  6. Quake (natural phenomenon) - Wikipedia

    en.wikipedia.org/wiki/Quake_(natural_phenomenon)

    An earthquake is a phenomenon that results from the sudden release of stored energy in the Earth's crust that creates seismic waves. At the Earth's surface, earthquakes may manifest themselves by a shaking or displacement of the ground and sometimes cause tsunamis, which may lead to loss of life and destruction of property. An earthquake is ...

  7. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. [2] A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface.

  8. Internal structure of Earth - Wikipedia

    en.wikipedia.org/wiki/Internal_structure_of_Earth

    The layering of Earth has been inferred indirectly using the time of travel of refracted and reflected seismic waves created by earthquakes. The core does not allow shear waves to pass through it, while the speed of travel (seismic velocity) is different in other layers.

  9. Elastic-rebound theory - Wikipedia

    en.wikipedia.org/wiki/Elastic-rebound_theory

    In geology, the elastic-rebound theory is an explanation for how energy is released during an earthquake. As the Earth's crust deforms, the rocks which span the opposing sides of a fault are subjected to shear stress. Slowly they deform, until their internal rigidity is exceeded.