enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Fault (geology) - Wikipedia

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

    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.

  3. Anderson's theory of faulting - Wikipedia

    en.wikipedia.org/wiki/Anderson's_Theory_of_Faulting

    Types 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. Transform fault - Wikipedia

    en.wikipedia.org/wiki/Transform_fault

    Diagram showing a transform fault with two plates moving in opposite directions Transform fault (the red lines). A transform fault or transform boundary, is a fault along a plate boundary where the motion is predominantly horizontal. [1]

  5. What causes earthquakes? The science behind why seismic ... - AOL

    www.aol.com/news/causes-earthquakes-science...

    Science & Tech. Sports. Weather. 24/7 Help. For premium support please call: ... On the West Coast, it can be possible to determine exactly which fault line a quake originated along, the USGS said ...

  6. Tilted block faulting - Wikipedia

    en.wikipedia.org/wiki/Tilted_block_faulting

    Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in extensional tectonic events, a result of tectonic plates stretching apart. [ 1 ] [ 2 ] When the upper lithospheric crust experiences extensional pressures, the brittle crust fractures, creating detachment faults . [ 3 ]

  7. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    Both compressional and extensional forces act along convergent boundaries. On the inner walls of trenches, compressional faulting or reverse faulting occurs due to the relative motion of the two plates. Reverse faulting scrapes off ocean sediment and leads to the formation of an accretionary wedge. Reverse faulting can lead to megathrust ...

  8. 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]

  9. Dangerous L.A. fault system rivaling the San Andreas tied to ...

    www.aol.com/news/recent-l-earthquakes-hit-along...

    Scientists believe the Puente Hills fault has a major quake roughly every few thousand years — but they don’t know when the last one was. The San Andreas fault has quakes more frequently; it ...