Plates are constantly in motion and are all moving at unique speeds. The African plate, for example, is moving at approximately 2.15 cm/year (about an inch/year), while the South American plate is moving at approximately 1.45 cm/year (about half an inch/year). Plates are constantly interacting at their boundaries. Scientists have identified three distinct kinds of plate boundaries, each of which interacts differently. These plate boundaries include divergent boundaries, convergent boundaries, and transform fault boundaries.
A divergent boundary represents an area where two plates are moving apart, or are diverging from one another. New magma from the mantle flows up to fill the space opened up by the plates moving apart. A narrow valley known as a rift valley usually forms in the space between the two plates as they pull apart. Since new crust is being created as a result of the plate motions, divergent boundaries are also known as constructive margins.
Divergent boundaries are usually found underwater as two plates of oceanic crust pull apart resulting in mid-oceanic ridges, but they can also be seen on land with two sections plates of continental crust moving apart.
The Red Sea was formed as a result of the African plate diverging from the Arabian plate.
It took over 100 million years for the Atlantic Ocean to assume its current shape.