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This process is called subduction.
A "subduction zone".
subduction is the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary.
When the oceanic plate sinks it is absorbed back into the magma.
, hot material rises towards the surface and cooler material sinks back down towards the Earth's core. This is called mantle convection and is driven by the heat generated from the Earth's core and the heat released from radioactive decay within the mantle. The motion of these convection currents is responsible for plate tectonics and the movement of continents over time.
This process is called subduction.
The plate with cooler, denser crust sinks under the other plate, forming a trench. There, the oceanic crust sinks down back into the mantle.
The plate with cooler, denser crust sinks under the other plate, forming a trench. There, the oceanic crust sinks down back into the mantle.
A "subduction zone".
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
subduction is the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary.
When the oceanic plate sinks it is absorbed back into the magma.
A "subduction zone".
A "subduction zone".
, hot material rises towards the surface and cooler material sinks back down towards the Earth's core. This is called mantle convection and is driven by the heat generated from the Earth's core and the heat released from radioactive decay within the mantle. The motion of these convection currents is responsible for plate tectonics and the movement of continents over time.
Hot, soft rock rise from the bottom of the mantle towards the top, cools, and sinks back through the mantle.
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