Mariana Trench Plates Involved In Its Formation. Such collisions involving subducting seamounts also. In this system, the western edge of one plate, the pacific plate, is subducted.
Mariana Trench Geology History Of Diving Museum
The mariana trench is formed by the process of subduction, where the pacific plate is forced beneath the mariana plate, a process known as the mariana trench subduction zone. Web the depth of the mariana trench varies along its length. Such collisions involving subducting seamounts also. In this system, the western edge of one plate, the pacific plate, is subducted. Web it is part of the western pacific system of oceanic trenches coinciding with subduction zones —points where two adjacent tectonic plates collide, one being forced below the other. Where large, old seamounts are present on the pacific plate at the subduction zone, the trench is shallower. It is separated from the philippine sea.
In this system, the western edge of one plate, the pacific plate, is subducted. The mariana trench is formed by the process of subduction, where the pacific plate is forced beneath the mariana plate, a process known as the mariana trench subduction zone. In this system, the western edge of one plate, the pacific plate, is subducted. Where large, old seamounts are present on the pacific plate at the subduction zone, the trench is shallower. Web it is part of the western pacific system of oceanic trenches coinciding with subduction zones —points where two adjacent tectonic plates collide, one being forced below the other. Web the depth of the mariana trench varies along its length. It is separated from the philippine sea. Such collisions involving subducting seamounts also.
