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  1. In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

  2. A fault is a fracture, or break, in the Earth's crust (lithosphere). Some faults are active. Here, sections of rock move past each other. This sometimes makes earthquakes. Faulting occurs when shear stress on a rock overcomes the forces which hold it together. The fracture itself is called a fault plane.

  3. en.wikipedia.org › wiki › FaultFault - Wikipedia

    Fault (computing), also called a trap or an exception, a type of interrupt in software or operating systems. Fault (technology), an abnormal condition or defect that may lead to a failure. Electrical fault, an abnormal current.

  4. This list covers all faults and fault-systems that are either geologically important [clarification needed] or connected to prominent seismic activity. [ clarification needed ] It is not intended to list every notable fault, but only major fault zones.

    Fault Name
    Length [km]
    Location
    Sense Of Movement
    Aedipsos-Kandili Fault
    60
    North Euboean Gulf, Greece
    Normal
    4000
    Kamchatka, Russia to Gulf of Alaska
    Subduction zone
    600
    South Island, New Zealand
    Dextral strike-slip (Transform)
    2000
    Tibetan Plateau / Tarim Basin
    Sinistral strike-slip
  5. Aug 28, 2024 · Fault, in geology, a planar or gently curved fracture in the rocks of Earth’s crust, where compressional or tensional forces cause relative displacement of the rocks on the opposite sides of the fracture. They range in length from a few centimeters to many hundreds of kilometers.

    • The Editors of Encyclopaedia Britannica
  6. In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

  7. www.wikiwand.com › simple › Fault_(geology)Fault (geology) - Wikiwand

    A fault is a fracture, or break, in the Earth's crust (lithosphere). Some faults are active. Here, sections of rock move past each other. This sometimes makes earthquakes.

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