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  2. Fault trace - Wikipedia

    en.wikipedia.org/wiki/Fault_trace

    A fault trace describes the intersection of a geological fault with the Earth's surface, which leaves a visible disturbance on the surface, usually looking like a crack in the surface with jagged rock structures protruding outward. The term also applies to a line plotted on a geological map to represent a fault.

  3. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. [3] [4] A fault zone is a cluster of parallel faults.

  4. List of fault zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fault_zones

    San Andreas Fault System (Banning fault, Mission Creek fault, South Pass fault, San Jacinto fault, Elsinore fault) 1300: California, United States: Dextral strike-slip: Active: 1906 San Francisco (M7.7 to 8.25), 1989 Loma Prieta (M6.9) San Ramón Fault: Chile: Thrust fault: Sawtooth Fault: Idaho, United States: Normal fault: Seattle Fault ...

  5. What the New Jersey earthquake tells us about the fault ... - AOL

    www.aol.com/news/jersey-earthquake-tells-us...

    The temblor, which measured 4.8 on the Richter scale, was considered a shallow earthquake by the U.S. Geological Survey, meaning that it occurred at a depth of zero to 70 kilometers below ground.

  6. Brothers Fault Zone - Wikipedia

    en.wikipedia.org/wiki/Brothers_Fault_Zone

    The Brothers Fault Zone (BFZ) is the most notable of a set of northwest-trending fault zones including the Eugene–Denio, McLoughlin, and Vale zones that dominate the geological structure of most of Oregon.

  7. Growth fault - Wikipedia

    en.wikipedia.org/wiki/Growth_fault

    Growth faults maturation is a long term process that takes millions of years with slip rate ranges between 0.2-1.2 millimeters per year. [4] [5] It starts when sedimentary sequences are deposited on top of each other above a thick evaporite layer (fig. 2). [6]

  8. New Madrid seismic zone - Wikipedia

    en.wikipedia.org/wiki/New_Madrid_Seismic_Zone

    The New Madrid seismic zone (NMSZ), sometimes called the New Madrid fault line (or fault zone or fault system), is a major seismic zone and a prolific source of intraplate earthquakes (earthquakes within a tectonic plate) in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri.

  9. Induced seismicity - Wikipedia

    en.wikipedia.org/wiki/Induced_seismicity

    Understanding the geological background on the site is a prerequisite for seismic hazard estimation. Formations of the rocks, subsurface structures, locations of faults, state of stresses and other parameters that contribute to possible seismic events are considered. Records of past earthquakes of the site are also taken into account. [81]