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  2. Rake (geology) - Wikipedia

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

    Rake (geology) In structural geology, rake (or pitch) is formally defined as "the angle between a line [or a feature] and the strike line of the plane in which it is found", measured on the plane. The three-dimensional orientation of a line can be described with just a plunge and trend. The rake is a useful description of a line because often ...

  3. Anderson's theory of faulting - Wikipedia

    en.wikipedia.org/wiki/Anderson's_Theory_of_Faulting

    Anderson's theory of faulting. Anderson's theory of faulting, devised by Ernest Masson Anderson in 1905, is a way of classifying geological faults by use of principal stress. [1][2] A fault is a fracture in the surface of the Earth that occurs when rocks break under extreme stress. [3] Movement of rock along the fracture occurs in faults.

  4. Fault (geology) - Wikipedia

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

    Fault (geology) Satellite image of a fault in the Taklamakan Desert. The two colorful ridges (at bottom left and top right) used to form a single continuous line, but have been split apart by movement along the fault. In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant ...

  5. What is the Almanor Fault Zone? Geologist explains region ...

    www.aol.com/news/almanor-fault-zone-geologist...

    A map by the California Geological Survey shows faults near the Lake Almanor area in Plumas County, where a magnitude 5.5 earthquake struck Thursday, May 11, 2023, followed by a magnitude 5.2 ...

  6. 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 ...

  7. Horst and graben - Wikipedia

    en.wikipedia.org/wiki/Horst_and_graben

    In geology, horst and graben (or range and valley) refers to topography consisting of alternating raised and lowered fault blocks known as horsts and grabens. The features are created by normal faulting and rifting caused by crustal extension. [1] Horst and graben are formed when normal faults of opposite dip occur in pairs with parallel strike ...

  8. 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 ...

  9. List of geological faults of England - Wikipedia

    en.wikipedia.org/wiki/List_of_geological_faults...

    This is a list of the named geological faults affecting the rocks of England. See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Many faults may have acted as both normal faults at one time and as ...