Diverging Plate Boundary
Subduction is a process that occurs when two oceanic plates pull apart
No, seafloor spreading does not hold the plates in place. Seafloor spreading is a process that occurs at mid-ocean ridges where new oceanic crust is formed and spreads apart. It is driven by the movement of tectonic plates, which are actually responsible for holding the seafloor in place.
Divergent Boundaries happen when two plates (oceanic or contental) begin to diverge, or move apart. Convergent Boundaries occur when two plates (again, oceanic or contential) begin to converge or move apart
The Mid-Atlantic Ridge.
New oceanic plates/crust are created in the space of separation.
Both continental and oceanic plates float on the top surface of the mantle, which is divided into convection cells. The movement of these convection cells drag the plates along: where convection causes the mantle material to fall the plates are pushed together and where convection causes the mantle material to rise the plates are pulled apart.
The movement of the hot mantle has broken the crust apart into large plates.
It represents the line of divergence (divergent plate margin) between oceanic plates, where two oceanic plates are moving apart and new oceanic crust is formed.
coenvergent zone
Oceanic trenches are the gaps which form when the tectonic plates move apart. They are the very deepest parts of the ocean.
where two plates pull apart from each other at oceanic ridges
Seafloor Spreading