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  • Subduction Zones: Where Oceanic Plates Meet and Melt
    The region where the seafloor and its sediments melt is called a subduction zone.

    Here's why:

    * Subduction: This process occurs when one tectonic plate (the denser oceanic plate) slides beneath another (the continental or less dense oceanic plate).

    * Melting: As the oceanic plate descends, it is subjected to intense pressure and heat from the Earth's mantle. These conditions cause the rock and sediments on the plate to partially melt.

    * Magma Generation: The melted rock forms magma, which is less dense than the surrounding solid rock. This magma rises towards the surface, often leading to volcanic activity.

    Therefore, subduction zones are areas where the seafloor and its sediments are subjected to the extreme conditions that cause melting and the formation of magma.

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