A divergent or constructive plate boundary. There can also be specific names like "a mid oceanic ridge" or a "rift valley".
Geologists call a crustal landmass that moves as a unit a tectonic plate. These plates float on the semi-fluid asthenosphere beneath them and interact at plate boundaries by either moving apart, colliding, or sliding past each other, leading to various geological phenomena.
The term for liquid rock is "magma" when it is beneath the Earth's surface and "lava" once it erupts onto the surface. Crustal plates float on the semi-fluid layer of the Earth known as the "asthenosphere," which is part of the upper mantle. This layer allows for the movement of tectonic plates above it.
Geologists call the process of tectonic plates breaking apart "rifting." It occurs when the Earth's lithosphere is being pulled apart, causing the plates to separate, creating new ocean basins. Rifting is a key stage in the formation of new tectonic boundaries.
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
divergent boundary
Tectonic plates.
When two plates move away from each other it is called a divergent plate boundary because they are dividing.
A deep valley where two tectonic plates move apart is called a rift valley. This occurs due to divergent plate tectonics, where the plates separate and magma rises to create new crust. Examples include the East African Rift Valley and the Mid-Atlantic Ridge.
Convergence Boundary.
divergent boundary
Tectonic plates are the moving irregularly shaped slabs that make up the Earth's lithosphere. These plates constantly shift and interact with each other, leading to phenomena such as earthquakes and volcanic activity.
A Tectonic Plate