Subduction is the process in plate tectonics where one tectonic plate is pushed beneath another into the mantle. This typically occurs where an oceanic plate meets a continental plate or another oceanic plate, resulting in the formation of deep oceanic trenches, volcanic arcs, and earthquakes. Subduction zones are important geologically as they are associated with the most powerful earthquakes and volcanic eruptions on Earth.
Subduction is the process where one tectonic plate moves beneath another plate at a convergent boundary. This often leads to the formation of deep ocean trenches and volcanic arcs due to the melting of the subducted plate under high pressure and temperature conditions. Subduction zones are known for generating earthquakes and volcanic activity.
A synonym for subduction is decrease.
Subduction is the process where one tectonic plate slides beneath another into the Earth's mantle at a convergent plate boundary. This process is responsible for the formation of deep ocean trenches, volcanic arcs, and earthquakes.
The process in which the ocean floor sinks into the mantle is called subduction. This occurs at convergent plate boundaries, where one tectonic plate slides beneath another. Subduction zones are associated with deep-sea trenches and volcanic activity.
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Related to plate subduction
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Subduction is the process where one tectonic plate moves beneath another plate at a convergent boundary. This often leads to the formation of deep ocean trenches and volcanic arcs due to the melting of the subducted plate under high pressure and temperature conditions. Subduction zones are known for generating earthquakes and volcanic activity.
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A synonym for subduction is decrease.
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