When oceanic crust is still young, it's relatively warm. The older it gets, the colder it gets. The colder it gets, the less volume it takes in, however, it's still the same amount of matter. This causes a bigger density, thus causing the crust to sink deeper into the mantle.
At the oceanic ridges the age of igneous basalt rocks is approximately zero (as that is where they formed) and the rocks get older the farther away.
The ages of sedimentary and metamorphic rocks does not correlate reliably with distance from the oceanic ridges like the ages of igneous rocks, because they can form anywhere not mainly at oceanic ridges. Igneous granite rocks are generally formed around continental volcanos not oceanic ridges.
Geologists have discovered that the deeper the ocean floor the older the crust. Conversely, the shallower the ocean floor, the younger the crust.
20 years
divergent boundary
divergent
A plate is not classified as convergent, divergent, or transform, a plate boundary i.e. a boundary between plates is. All three types of plate boundary can be found along the edges of the North American plate.
They are divergent plates
It is a rift zone or a divergent boundary. plus. no offense to that person that uploaded the previous answer.
Convergent on the western perimeter, divergent on the Easter perimeter.
Convergent: plates move into one another.Divergent: plates move apart.Transform: plates move sideways in relation to each other.
divergent boundary
Divergent, convergent and transform.
divergent boundary
Divergent Boundaries - A boundary between two lithoperic plates that are moving apart .
divergent boundary
a divergent plate boundary.
The Andes are a result of the convergent boundary between the Nazca and South American Plate.
It is a transform boundary.
divergent boundary
They are divergent plates