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  2. 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]

  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. Epicenter - Wikipedia

    en.wikipedia.org/wiki/Epicenter

    Earthquakes. The epicenter (/ ˈɛpɪˌsɛntər /), epicentre, or epicentrum[1] in seismology is the point on the Earth 's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates.

  5. 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.

  6. Seismic wave - Wikipedia

    en.wikipedia.org/wiki/Seismic_wave

    A seismic wave is a mechanical wave of acoustic energy that travels through the Earth or another planetary body. It can result from an earthquake (or generally, a quake), volcanic eruption, magma movement, a large landslide and a large man-made explosion that produces low-frequency acoustic energy.

  7. Focal mechanism - Wikipedia

    en.wikipedia.org/wiki/Focal_mechanism

    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 ...

  8. Deep-focus earthquake - Wikipedia

    en.wikipedia.org/wiki/Deep-focus_earthquake

    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 ...

  9. Epicentral distance - Wikipedia

    en.wikipedia.org/wiki/Epicentral_distance

    Earthquakes. Epicentral distance refers to the ground distance from the epicenter to a specified point. [1] Generally, the smaller the epicentral distance of an earthquake of the same scale, the heavier the damage caused by the earthquake. On the contrary, with the increase of epicentral distance, the damage caused by the earthquake is ...