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  2. List of tectonic plate interactions - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plate...

    Convergent boundaries are areas where plates move toward each other and collide. These are also known as compressional or destructive boundaries. Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This ...

  3. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    A convergent boundary (also known as a destructive boundary) is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other, a process known as subduction. The subduction zone can be defined by a plane where many earthquakes occur, called the Wadati–Benioff zone. [1]

  4. List of tectonic plates - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plates

    For purposes of this list, a major plate is any plate with an area greater than 20 million km 2 (7.7 million sq mi) African plate – Tectonic plate underlying Africa – 61,300,000 km 2 (23,700,000 sq mi) Antarctic plate – Major tectonic plate containing Antarctica and the surrounding ocean floor – 60,900,000 km 2 (23,500,000 sq mi)

  5. List of megathrust earthquakes - Wikipedia

    en.wikipedia.org/wiki/List_of_megathrust_earthquakes

    Comparison of recent and historic earthquakes by energy release. Megathrust earthquakes are large seismic events that take place along convergent plate boundaries, particularly at subduction zones. Examples of subduction zones include the Sumatra and Java trenches, Nankai Trough and Peru–Chile Trench which are frequent sources of these ...

  6. Megathrust earthquake - Wikipedia

    en.wikipedia.org/wiki/Megathrust_earthquake

    Megathrust earthquakes occur at convergent plate boundaries, where one tectonic plate is forced underneath another. The earthquakes are caused by slip along the thrust fault that forms the contact between the two plates. These interplate earthquakes are the planet's most powerful, with moment magnitudes (M w) that can exceed 9.0.

  7. List of fault zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fault_zones

    Associated earthquakes Sources Aedipsos-Kandili Fault: 60: North Euboean Gulf, Greece: Normal: Active: Alaska–Aleutian megathrust: 4000: Kamchatka, Russia to Gulf of Alaska: Subduction zone: Active: 1964 Prince William Sound (M9.2), 1965 Rat Islands (M8.7), 1957 Andreanof Islands (M8.6) [1] Alpine Fault: 600 South Island, New Zealand: Dextral ...

  8. Organizations that took a stand amidst the disaster of ...

    www.aol.com/news/2015-08-28-organizations-that...

    The hurricane brought death, destroyed homes and belongings, and caused indescribable pain. The situation seemed hopefully for many, but several charities and organizations -- both big and small ...

  9. Submarine earthquake - Wikipedia

    en.wikipedia.org/wiki/Submarine_earthquake

    Tectonic plate boundaries, showing the directions of plate movements. Different kinds of boundaries. The different ways in which tectonic plates rub against each other under the ocean or sea floor to create submarine earthquakes. The type of friction created may be due to the characteristic of the geologic fault or the