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These are areas where one plate is submerging to the other, being pulled down into the mantle.

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What deep ocean feature form at subduction zones?

Trenches are deep ocean features of subduction zones.


What is the process in which the ocean floor sinks into the mantle is called?

The process in which the ocean floor sinks into the mantle is called subduction. This occurs at convergent plate boundaries, where one tectonic plate slides beneath another. Subduction zones are associated with deep-sea trenches and volcanic activity.


A deep trench in the earth is called?

subduction


What are the deepest part of the ocean floor?

The deepest parts of the ocean floor are caused by plate tectonic subduction and occur where the sea floor sinks back into the mantle in a subduction zone. These areas are called deep sea trenches and the Challenger Deep in the Mariana Trench in the Pacific is the deepest known point in Earth's oceans.


What deep feature is found at subduction zone?

Trench


What process produceces deep sea trenches?

Subduction.


What events commonly occurs at subduction zones?

Earthquakes, volcanic eruptions, and the formation of deep ocean trenches commonly occur at subduction zones. The subduction of one tectonic plate beneath another can trigger these events due to the intense geologic activity and pressure present in these areas.


Areas where earthquake occurs?

subduction zones


What produces deep sea trenches?

A process known as subduction creates deep sea trenches.


What is the region where oceanic lithosphere sinks into the asthenosphere?

This process occurs at subduction zones, where one tectonic plate descends beneath another plate into the asthenosphere. Subduction zones are typically associated with deep ocean trenches and volcanic arcs.


What are deep underwater canyon?

They are created in a process known as, subduction.


The deepest earthquakes tend to occur at?

subduction zones, where tectonic plates collide or slide past each other. Subduction zones are characterized by deep-seated forces that generate powerful earthquakes deep within the Earth's crust. These deep earthquakes can reach depths of 700 kilometers or more.