Most divergent plates are at oceanic plate boundaries. This is where long chains of underwater volcanoes spew out lava.
And it turns out, these mid-oceanic ridges (rift valleys) has the youngest geologic rocks on the planet. Generally, ocean floor consists of mostly igneous rocks “basalt” which spread at these mid-oceanic ridges.
Plates move apart at divergent boundaries
Beneath the oceans, lava erupts every day. Because it’s all underground, we don’t realize it’s even happening.
Actually, the Earth has 70,000 km of continuous volcanoes under the ocean. More specifically, the volcanoes are at mid-oceanic ridges. If you took all the water away from the oceans, it would be the most prominent feature on Earth.
Plate tectonics begin at mid-oceanic ridges where plates are moving apart. Because plates pull apart from each other at divergent plates, lava spews out to create the youngest geological rocks on Earth.
Divergent boundaries map
Here are examples of where we can find divergent plate boundaries:
- ATLANTIC OCEAN: A divergent plate boundary runs for most of the length of the Atlantic Ocean. This is the longest divergent plate on the planet.
- AFRICAN PLATE: The African Plate is in the process of rifting apart into two separate plates where it will become ocean. In addition, the Somalian and Nubian plates will one day tear apart and become new ocean.
- RED SEA: Between Asia and Africa, the Red Sea is spreading apart from the African and Arabian Plates.
The youngest rock form at divergent plate boundaries
Hidden beneath Earth’s oceans, underwater volcanoes spew out lava at mid-oceanic ridges (rift valleys).
Because divergent plates move apart from each other at these mid-oceanic ridges, magma flows upwards from the mantle beneath.
When the lava hardens, it becomes dark igneous rock or “basalt” at rift volcanoes.
Because divergent plates fill in the gaps with basalt, oceanic crust turns out to be very young geologically.
Over time, the plates grow at oceanic crust and older rock is pushed away from mid-oceanic ridges.