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  2. Blind thrust earthquake - Wikipedia

    en.wikipedia.org/wiki/Blind_thrust_earthquake

    [3] [4] A NASA study which combined satellite radar images and Global Positioning System (GPS) observations found that "tectonic squeezing across Los Angeles" "will likely produce earthquakes on either the blind Elysian Park or Puente Hills thrust fault systems". [5] A blind thrust earthquake along the Puente Hills fault could contribute more ...

  3. Northridge Blind Thrust Fault - Wikipedia

    en.wikipedia.org/wiki/Northridge_Blind_Thrust_Fault

    The Northridge Blind Thrust Fault (also known as the Pico Thrust Fault) is a thrust fault that is located in the San Fernando Valley area of Los Angeles.It is the fault that triggered the M w 6.7 1994 Northridge earthquake which caused $13–50 billion in property damage (equivalent to 24–93 billion today) and was one of the costliest natural disasters in U.S. history.

  4. Thrust fault - Wikipedia

    en.wikipedia.org/wiki/Thrust_fault

    Thrust fault in the Qilian Shan, China.The older (left, blue, and red) thrust over the younger (right, brown). The Glencoul Thrust at Aird da Loch, Assynt in Scotland. The irregular grey mass of rock is formed of Archaean or Paleoproterozoic Lewisian gneisses thrust over well-bedded Cambrian quartzite, along the top of the younger unit.

  5. Elysian Park Fault - Wikipedia

    en.wikipedia.org/wiki/Elysian_Park_Fault

    Elysian Park Fault is an active blind thrust fault located in Central Los Angeles, California.Approximately 20 km (12.4 miles) long, the fault is believed to able to produce a destructive earthquake of magnitude 6.2–6.7, about every 500–1,300 years, similar in size and frequency to the 1971 San Fernando earthquake or 1994 Northridge earthquake.

  6. Thrust tectonics - Wikipedia

    en.wikipedia.org/wiki/Thrust_tectonics

    Thrust tectonics or contractional tectonics is concerned with the structures formed by, and the tectonic processes associated with, the shortening and thickening of the crust or lithosphere. It is one of the three main types of tectonic regime, the others being extensional tectonics and strike-slip tectonics .

  7. Megathrust earthquake - Wikipedia

    en.wikipedia.org/wiki/Megathrust_earthquake

    A thrust fault is a type of reverse fault, in which the rock above the fault is displaced upwards relative to the rock below the fault. This distinguishes reverse faults from normal faults , where the rock above the fault is displaced downwards, or strike-slip faults , where the rock on one side of the fault is displaced horizontally with ...

  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. Fold mountains - Wikipedia

    en.wikipedia.org/wiki/Fold_mountains

    Fold mountains form in areas of thrust tectonics, such as where two tectonic plates move towards each other at convergent plate boundary.When plates and the continents riding on them collide or undergo subduction (that is – ride one over another), the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak ...