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  2. 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]

  3. 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]

  4. 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 .

  5. Earthquake - Wikipedia

    en.wikipedia.org/wiki/Earthquake

    The initial point of rupture is called the hypocenter or focus, while the ground level directly above it is the epicenter. Earthquakes are primarily caused by geological faults, but also by volcanism, landslides, and other seismic events. The frequency, type, and size of earthquakes in an area define its seismic activity, reflecting the average ...

  6. Focal mechanism - Wikipedia

    en.wikipedia.org/wiki/Focal_mechanism

    The data for an earthquake is plotted using a lower-hemisphere stereographic projection. The azimuth and take-off angle are used to plot the position of an individual seismic record. The take-off angle is the angle from the vertical of a seismic ray as it emerges from the earthquake focus.

  7. Epicenter - Wikipedia

    en.wikipedia.org/wiki/Epicenter

    The point at which fault slipping begins is referred to as the focus of the earthquake. [8] The fault rupture begins at the focus and then expands along the fault surface. The rupture stops where the stresses become insufficient to continue breaking the fault (because the rocks are stronger) or where the rupture enters ductile material. [8]

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  9. Focus - Wikipedia

    en.wikipedia.org/wiki/Focus

    Focus (earthquake), an earthquake's underground point of origin or hypocenter Focus (optics) , a point toward which rays are made to converge Military technology