What geological feature is formed at divergent boundaries?

Divergent boundaries are locations where tectonic plates move away from each other, leading to the formation of new crust. As the plates separate, magma rises from the mantle to fill the gap, solidifying to create new oceanic crust. This process is most commonly observed at mid-ocean ridges. These ridges are characterized by volcanic activity and the formation of underwater mountains as new materials are added to the ocean floor. This creation of new crust at divergent boundaries is essential to understanding the dynamic processes that shape the Earth's surface and is a key part of the plate tectonics theory. In contrast, other geological features like mountains and subduction zones are associated with convergent or transform boundaries, where different tectonic interactions occur.