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  2. Aleutian subduction zone - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Subduction_Zone

    Here, the Pacific Plate is being subducted underneath the North American Plate and the rate of subduction changes from west to east from 7.5 to 5.1 cm (3.0 to 2.0 in) per year. [2] The Aleutian subduction zone includes two prominent features, the Aleutian Arc and the Aleutian Trench. The Aleutian Arc was created via volcanic eruptions from ...

  3. Aleutian Trench - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Trench

    The Aleutian Trench (or Aleutian Trough) [1] is an oceanic trench along a convergent plate boundary which runs along the southern coastline of Alaska and the Aleutian islands. The trench extends for 3,400 kilometres (2,100 mi) from a triple junction in the west with the Ulakhan Fault and the northern end of the Kuril–Kamchatka Trench , to a ...

  4. Denali Fault - Wikipedia

    en.wikipedia.org/wiki/Denali_Fault

    Tectonic map of Alaska and northwestern Canada showing main faults and historic earthquakes Denali Fault and the Denali National Park boundary. The Denali Fault is a major intracontinental dextral (right lateral) strike-slip fault in western North America, extending from northwestern British Columbia, Canada to the central region of the U.S. state of Alaska.

  5. Queen Charlotte Fault - Wikipedia

    en.wikipedia.org/wiki/Queen_Charlotte_Fault

    Tectonic map of Alaska and northwestern Canada showing main faults and historic earthquakes. The Queen Charlotte Fault is an active transform fault that marks the boundary of the North American plate and the Pacific plate. [1] [2] It is Canada's right-lateral strike-slip equivalent to the San Andreas Fault to the south in California. [3]

  6. 1964 Alaska earthquake - Wikipedia

    en.wikipedia.org/wiki/1964_Alaska_earthquake

    The Alaska earthquake was a subduction zone (megathrust) earthquake, caused by an oceanic plate sinking under a continental plate. The fault responsible was the Aleutian Megathrust , a reverse fault caused by a compressional force.

  7. Aleutian Arc - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Arc

    The Aleutian Trench, formed by the subduction of the Pacific plate under the North American plate, sits south of the island arc. [2] A forearc basin reaching depths of 7 km occupies the space between the trench and the island arc and leads up to the Aleutian Ridge, the north side of which being the area where the most volcanic activity occurs. [2]

  8. List of fault zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fault_zones

    Subduction zone (continental collision) Active: 1505 Lo Mustang (M8.9), 1950 Assam-Tibet (M8.6) 2015 Gorkha (M7.8), 2015 Nepal (M7.3) Main Uralian Fault (MUF) 2000+ Urals: Subduction zone: Marianna Fault: Arkansas, United States: Marikina Valley fault system: Philippines: Dextral strike-slip: Active: Marlborough fault system: South Island, New ...

  9. Geology of the Pacific Ocean - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Pacific_Ocean

    Related causes of island formation include obduction and subduction at convergent plate boundaries. Malaita and Ulawa in the Solomon Islands are the result of obduction while the effects of subduction can be seen in the formation of volcanic island arcs such as the Aleutian Arc off Alaska and the Kermadec-Tonga Subduction Zone north of New ...