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  2. Deep-focus earthquake - Wikipedia

    en.wikipedia.org/wiki/Deep-focus_earthquake

    A deep-focus earthquake in seismology (also called a plutonic earthquake) is an earthquake with a hypocenter depth exceeding 300 km. They occur almost exclusively at convergent boundaries in association with subducted oceanic lithosphere .

  3. Depth of focus (tectonics) - Wikipedia

    en.wikipedia.org/wiki/Depth_of_focus_(tectonics)

    In seismology, the depth of focus or focal depth is the depth at which an earthquake occurs. Earthquakes occurring at a depth of less than 70 km (43 mi) are classified as shallow-focus earthquakes, while those with a focal depth between 70 km (43 mi) and 300 km (190 mi) are commonly termed mid-focus or intermediate-depth earthquakes. [1]

  4. Subduction zone metamorphism - Wikipedia

    en.wikipedia.org/wiki/Subduction_zone_metamorphism

    Transition into the eclogite facies is proposed to be the source of earthquakes at depths greater than 70 km. These earthquakes are caused by the contraction of the slab as minerals transition into more compact crystal structures. The depth of these earthquakes on the subducting slab is known as the Wadati–Benioff zone. [22]

  5. Wadati–Benioff zone - Wikipedia

    en.wikipedia.org/wiki/Wadati–Benioff_zone

    In 1949, Hugo Benioff introduced a method for determining elastic-rebound strain increments of earthquakes on a particular fault. [5] He determined that the square root of an earthquake's energy is proportional to both the elastic rebound strain increment and the rebound displacement, and developed a way to determine whether a series of earthquakes was generated along a single fault structure.

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

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

    Moderately damaging earthquakes strike between New York and Wilmington, Delaware, about twice a century, the USGS said, and smaller earthquakes are felt in the region roughly every two to three years.

  7. Seismogenic layer - Wikipedia

    en.wikipedia.org/wiki/Seismogenic_layer

    This can result in extremely deep earthquakes up to 700 kilometres (430 mi) in depth. [3] The base of this layer represents the downwards change in deformation mechanism from elastic and frictional processes (associated with brittle faulting) to a generally aseismic zone where ductile creep becomes the dominant process.

  8. Magnitude 6.9 earthquake hits southern Japan, tsunami ... - AOL

    www.aol.com/magnitude-6-9-earthquake-hits...

    Data provided by USGS showed the earthquake was just over 22 miles deep. Tsunami advisories for waves up to about 3.5 feet were issued for the southern prefectures of Miyazaki and Kochi, online ...

  9. Odd 4.5-magnitude earthquake reported in deep ocean ... - AOL

    www.aol.com/odd-4-5-magnitude-earthquake...

    A strong 4.5-magnitude earthquake occurred in deep waters off the North Carolina coast Wednesday, April 19, according to the U.S. Geological Survey.. It happened shortly after noon and witnesses ...