An oceanic plate can descend beneath another oceanic plate - Japan, Indonesia, and the Aleutian Islands are examples of this type of subduction. Alternately, an oceanic plate can descend beneath a continental plate - South America, Central America, and the Cascade Volcanoes are an example of this type of subduction.
two examples are the Juan de fuca and the north American plate.
two examples are the Juan de fuca and the north American plate.
A synonym for subduction is decrease.
That is the correct spelling of "subduction."
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.
It is known as subduction.
Subduction.
the subduction volcano is found where
Moun Cleveland formed as a result of a subduction zone, but is not a subduction zone in and of itself. A subduction zone is a feature that forms volcanoes, not a kind of volcano.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
Frequent earthquakes occur at subduction zones where one tectonic plate is being forced beneath another. These earthquakes are caused by the intense pressure and friction between the plates as they move against each other. Examples of subduction zones with frequent earthquakes include the Pacific Ring of Fire where the Pacific Plate is subducting beneath other plates.
subduction zone