No. While only oceanic crust can subduct it is not always subducting. When two oceanic plates converge, only one of them subducts.
When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.
An ocean plate is subducting if it is flowing under a less dense plate at a convergent plate boundary.
If the plates are moving toward each other, the more dense oceanic plate will subduct underneath the less dense continental plate. Mountain ranges and volcanism may result as the water saturated subducting oceanic crust creates molten rock which attempts to rise to the surface.
oceanic crust and continental crust collide, with the continental crust subducting under the oceanic
It is oceanic
A series of volcanic islands formed by an older oceanic plate subducting under a newer oceanic plate.
When an oceanic plate goes under a continental plate, the subducting plate ---> oceanic creates a curved line of volcanoes along the edge of the overlying continental plate.
Convergent with the oceanic plate subducting under the continental plate.
When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.
When an oceanic plate subducts below another continental or oceanic plate, the cold, wet, dense rock and sediments slowly dive into the asthenosphere, where, due to the volume of water contained in the subducting plate, the melting point of the subducting plate is lower than the surrounding rock. Volcanoes may result from the rising of molten material created by the subduction.
It was formed from the volcanism created by a subducting oceanic plate at a convergent plate boundary.
In a oceanic-continentalconvergent boundaryyou normally get subduction , when one plate slides under another. In this case the plate subducting, or going under is the oceanic plate ( it is more dense ), so the mountains would be just of the continental plate. In aoceanic-oceanic convergent boundary the mountains would just be oceanic ( basalt).
The oldest layers of sea floor would exist at the bottom of the Marianas Trench, where oceanic plate subduction is occurring. The subducting oceanic plate is less than 200 million years in age.
An ocean plate is subducting if it is flowing under a less dense plate at a convergent plate boundary.
The Andes Mountain Range is a result of the Nazca Plate subducting under the South American Plate.
In the scope of lithospheric plate movements, both boundaries are areas where the more dense of the colliding plates slides under the lighter one, and moves toward the mantle. The melting of the subducted crust as it nears the mantle may cause volcanism either on the sea floor or on the continental land mass. Earthquakes will also result as the subducting rocks break and grind their way past the non-subducting plate rock.
Nazca