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  2. Deep-focus earthquake - Wikipedia

    en.wikipedia.org/wiki/Deep-focus_earthquake

    Seismicity cross-section across part of the Kuril Islands subduction zone. Many deep earthquakes have occurred. 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)

    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 ...

  4. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    An earthquake – also called a quake, tremor, or temblor – is the shaking of the Earth 's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes can range in intensity, from those so weak they cannot be felt, to those violent enough to propel objects and people into the air, damage ...

  5. Seismology - Wikipedia

    en.wikipedia.org/wiki/Seismology

    Seismology (/ saɪzˈmɒlədʒi, saɪs -/; from Ancient Greek σεισμός (seismós) meaning "earthquake" and -λογία (-logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through the Earth or other planetary bodies. It also includes studies of ...

  6. Wadati–Benioff zone - Wikipedia

    en.wikipedia.org/wiki/Wadati–Benioff_zone

    Wadati–Benioff zone. A Wadati–Benioff zone (also Benioff–Wadati zone or Benioff zone or Benioff seismic zone) is a planar zone of seismicity corresponding with the down-going slab in a subduction zone. [1] Differential motion along the zone produces numerous earthquakes, the foci of which may be as deep as about 670 km (420 mi).

  7. Seismic magnitude scales - Wikipedia

    en.wikipedia.org/wiki/Seismic_magnitude_scales

    Seismic magnitude scales are used to describe the overall strength or "size" of an earthquake. These are distinguished from seismic intensity scales that categorize the intensity or severity of ground shaking (quaking) caused by an earthquake at a given location. Magnitudes are usually determined from measurements of an earthquake's seismic ...

  8. Shallow focus - Wikipedia

    en.wikipedia.org/wiki/Shallow_focus

    Shallow focus is a photographic and cinematographic technique incorporating a small depth of field. In shallow focus, one plane of the scene is in focus while the rest is out of focus. Shallow focus is typically used to emphasize one part of the image over another. [1] Photographers sometimes refer to the aesthetic quality of the unfocused area ...

  9. Hypocenter - Wikipedia

    en.wikipedia.org/wiki/Hypocenter

    Hypocenter (Focus) and epicenter of an earthquake. An earthquake's hypocenter or focus is the position where the strain energy stored in the rock is first released, marking the point where the fault begins to rupture. [3] This occurs directly beneath the epicenter, at a distance known as the hypocentral depth or focal depth. [3]