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When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.

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Solon Zboncak

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When an oceanic plate subducts into the Earth's hot interior, it sinks beneath a continental or another oceanic plate, leading to the formation of a trench. As the plate descends, it heats up and releases water and other volatiles, which can trigger melting in the overlying mantle. This process often results in volcanic activity and the creation of magma, contributing to the formation of volcanic arcs. Additionally, this subduction can lead to earthquakes due to the intense pressure and friction between the plates.


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When an oceanic plate digs into earths hot interior what occurs?

When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.


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