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  2. List of tectonic plate interactions - Wikipedia

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

    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 causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]

  3. Silfra - Wikipedia

    en.wikipedia.org/wiki/Silfra

    Silfra fissure The Mid-Atlantic Ridge passing through Þingvellir Rocks and boulders that have piled up in the fissure due to earthquakes.. Silfra (Icelandic pronunciation: [ˈsɪl(v)ra]) is a rift formed in the Mid-Atlantic Ridge – the divergent tectonic boundary between the North American and Eurasian plates – and is located in the Þingvallavatn Lake in the Þingvellir National Park in ...

  4. Cave diving regions of the world - Wikipedia

    en.wikipedia.org/wiki/Cave_diving_regions_of_the...

    It is the only place in the world where you can dive or snorkel directly in a crack between two tectonic plates. [22] The tunnel from the entrance of Silfra to the cave is commonly known as ‘The Tunnel’, due to the strong current that ‘flushes’ divers attempting to swim through.

  5. The Earth's tectonic plates made the Himalayas — and could ...

    www.aol.com/news/earth-tectonic-plates-made...

    In the heart of Asia, deep underground, two huge tectonic plates are crashing into each other — a violent but slow-motion bout of geological bumper cars that over time has sculpted the soaring ...

  6. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    The motivating force for seafloor spreading ridges is tectonic plate slab pull at subduction zones, rather than magma pressure, although there is typically significant magma activity at spreading ridges. [3] Plates that are not subducting are driven by gravity sliding off the elevated mid-ocean ridges a process called ridge push. [4]

  7. Mariana Trench - Wikipedia

    en.wikipedia.org/wiki/Mariana_Trench

    The Mariana Trench is part of the Izu–Bonin–Mariana subduction system that forms the boundary between two tectonic plates. In this system, the western edge of one plate, the Pacific plate, is subducted (i.e., thrust) beneath the smaller Mariana plate that lies to the west.

  8. New York is shook. But how can an earthquake hit in the ... - AOL

    www.aol.com/finance/york-shook-earthquake-hit...

    Your teacher might have said they occur where two tectonic plates meet, at a fault line, as the plates slide against each other, separate, or converge. ... Faults don’t just exist between major ...

  9. Divergent boundary - Wikipedia

    en.wikipedia.org/wiki/Divergent_boundary

    This is an accepted version of this page This is the latest accepted revision, reviewed on 17 January 2025. Linear feature that exists between two tectonic plates that are moving away from each other This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources ...

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