Which feature is commonly associated with divergent plate boundaries?

Divergent plate boundaries are characterized by tectonic plates moving away from each other. As these plates separate, magma from the mantle rises to fill the gap, leading to the formation of new oceanic crust. This process typically generates mid-ocean ridges, which are underwater mountain ranges created by the upwelling of magma. These ridges are the sites of significant volcanic activity and are critical to the theory of plate tectonics, as they help demonstrate how new ocean crust is formed and how plates interact.

Mid-ocean ridges illustrate the dynamic nature of the Earth's crust at divergent boundaries, highlighting the creation of features like rift valleys and the associated seismic activity. This is contrasted with other geological features that are more common at convergent boundaries, such as mountain ranges formed by the collision of tectonic plates, ocean trenches that are the result of subduction, and volcanic arcs associated with the subduction of oceanic plates beneath continental plates. Each of these features represents different tectonic activities and processes, thus clarifying why mid-ocean ridges are the hallmark of divergent boundaries.