Tectonic
Subduction is a process that occurs when two oceanic plates pull apart
The oceanic plate subducts under the continental because it is denser. The Andes are being formed in this way and the Himalayas started that way also.
It subducts under another
This is called a destructive plate boundary. It occurs due to the fact that the oceanic crust is far denser than the continental crust. As a result it subducts into the mantle and is incenerated. Hope it helped:)
Everytime a volcano erupts, the magma gets higher and higher everytime it hardens. This causes an island arc
It subducts under the continental plate because the oceanic plate is denser.
the oceanic plate subducts under the continental plate and then melts in the mantle and often will create volcanos along the conitinental plate.\
the oceanic plate subducts under the continental plate and then melts in the mantle and often will create volcanos along the conitinental plate.\
Subduction is a process that occurs when two oceanic plates pull apart
No. In addition to oceanic crust being created at mid-ocean ridges, crust is destroyed at certain convergent plate boundaries where one plate subducts under another.
The oceanic plate subducts under the continental because it is denser. The Andes are being formed in this way and the Himalayas started that way also.
The oceanic plate subducts under the continental because it is denser. The Andes are being formed in this way and the Himalayas started that way also.
This happens at a plate boundary. The oceanic plate subducts (sinks) under the continental plate, because it is heavier. (the oceanic plate is made of basalt and the continental plate is made of granite.) This happens at a destructive plate margin. it is called this because part if the oceanic plate is destroyed, because it melts as it sinks.
It subducts under another
Trenches are formed at convergent plate boundaries involving at least one oceanic plate, where the more dense plate subducts under the less dense plate.
The more dense plate subducts (goes under) the less dense plate. For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
Usually when it meets another tectonic plate at a convergent plate boundary. If the oceanic plate converges with a continental plate the denser oceanic plate will be forced under the continental plate. If it converges with another oceanic plate the older (and therefore cooler and denser) plate will be forced under the younger plate.