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Subduction plays a crucial role in the rock cycle by facilitating the recycling of Earth's materials. When tectonic plates converge, one plate often sinks beneath another into the mantle, where it melts and transforms into magma. This process not only contributes to the formation of igneous rocks when the magma is extruded, but it also leads to the metamorphism of existing rocks due to the extreme heat and pressure conditions in subduction zones. Ultimately, subduction helps to drive the continuous transformation and movement of rocks within the rock cycle.

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During subduction, one tectonic plate moves beneath another into the mantle. This process can cause melting of the descending plate, leading to the formation of magma. This magma can then rise to the surface through volcanic activity, contributing to the formation of new igneous rocks and completing the rock cycle.


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Subduction in the rock cycle refers to the process where one tectonic plate moves underneath another at a convergent boundary. As the plates collide, the denser oceanic plate sinks into the mantle, leading to the recycling of crustal material back into the Earth's interior. This process plays a crucial role in the formation of volcanic arcs and mountain ranges.


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Subduction zones forces rocks to be pulled back down into the mantle where pressure and heat melts and recycles the rocks. Convection in the mantle then forces the magma to the surface at mid ocean ridges and volcanoes.


How is lgneous rock and sedimentary rock and metomorphic rock is the same?

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