The Process By Which The Ocean Floor Sinks Beneath

The process where the ocean floor sinks beneath the crust and back into the mantle is known as subduction.

The process by which the ocean floor sinks beneath.

This is the result of the collision of two tectonic plates. Where there are trenches subduction takes place. The lava spreads out pushing older rocks aside. This in turn results in the.

Most geologists think that the movement of earth s plates is caused by. Describe the process of sea floor spreading. Where does the salt in the ocean come from. Sea floor spreading and subduction work together.

Ocean floor is made of which igneous rock. The ocean floor does not just keep spreading. The process of what continually adds new crust to the ocean floor along both sides of the mid ocean ridge. The process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle rift valley a deep valley that forms on land at a divergent boundary where two plates move apart.

The process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle is known as. Subduction is the process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle. The scientist who created the seafloor spreading theory was hint. Deep valley or underwater canyon where the oceanic crust sinks back toward the mantle.

The process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle is known as. As subduction occurs crust closer to a mid ocean ridge moves away from the ridge and toward a deep ocean trench. The process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle. The process by which the ocean floor sinks beneath continental crust at a deep ocean trench and back into the mantle is known as.

The process of adding more crust to the ocean floor. Molten material rises from the mantle and erupts through the mid ocean ridge. The process by which ocean floor sinks beneath a deep ocean trench and back into the mantle is called subduction sub duk shun. Convection currents under the lithosphere push new crust that forms at the mid ocean ridge away from the ridge and toward a deep ocean trench.

Subduction is the process by which the ocean floor sinks beneath a deep ocean trench and back into the mantle to be recycled.