What is the movement direction of divergent boundaries?

Divergent boundaries are characterized by tectonic plates moving apart from each other. This movement typically occurs at mid-ocean ridges, where new oceanic crust is formed as magma rises from the mantle. As the plates separate, magma fills the gap, resulting in volcanic activity and the creation of new seafloor. This process not only shapes the ocean floor but also influences geological features, such as rift valleys and increased seismic activity in these regions. The movement of tectonic plates away from one another is fundamental to the theory of plate tectonics, making the understanding of divergent boundaries essential in studying geological and oceanographic processes.