No. Diverging means "moving apart." Subduction occurs at convergent plate boundaries, where two plates come together and one slides under the other.
The older denser plate sinks under a deep ocean trench into the mantle. Some rock above the subducting plate melts and forms magma. Since the magma is less dense than the surrounding rock, it rises toward the surface. Eventually, the magma breaks through the ocean floor, making a volcanoe.
Subduction zones are found near convergent plate boundaries, where two tectonic plates collide and one plate is forced beneath the other, leading to the formation of deep ocean trenches and volcanic arcs.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
A trench or subduction zone develops at plate boundaries where one oceanic plate descends beneath another. This process is called subduction and typically results in the formation of deep oceanic trenches and volcanic arcs due to melting of the descending plate.
The region is called a subduction zone. It occurs at convergent plate boundaries where one tectonic plate is forced below another due to differences in density. This subduction process can lead to volcanic activity and earthquakes.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
Submarine volcanoes.
Diverging tectonic plates.
At diverging plate boundaries, new oceanic crust forms through seafloor spreading. Magma rises to the surface and solidifies, creating mid-ocean ridges. As the plates move apart, they create new oceanic crust, which can lead to the formation of rift valleys.
Subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate.
A subduction zone is where one plate is being subducted ( pulled down) under another plate, No it is not a plate boundary but it is were it happens. hope this helps
Most are found on converging
The older denser plate sinks under a deep ocean trench into the mantle. Some rock above the subducting plate melts and forms magma. Since the magma is less dense than the surrounding rock, it rises toward the surface. Eventually, the magma breaks through the ocean floor, making a volcanoe.
Subduction zones form along some tectonic plate boundaries. Of the three general types of tectonic plate boundaries, we will see them form at some (but not all) of what are called convergent plate boundaries.
Continental and Oceanic plates.
Converging (destructive) plate boundary: where two plates collide. Diverging (constructive) plate boundary: where two plates move away from each other. Transform plate boundary: where two plates move, or grind, past each other. Like the boundary in California.
In plate tectonics, when two tectonic plates move toward each other, it results in the formation of what is called a convergent plate boundary. The two plates are said to converge. One plate may be more dense than the other, and with the two plates pushing against each other, the plate that is more dense will "slide under" the other plate. The plate sliding under is said to subduct the other plate, and this creates what is called a subduction zone. Not all convergent plate boundaries have subduction zones, but all subduction zones are formed at convergent plate boundaries.