Which landform is commonly associated with divergent plate boundaries?

Divergent plate boundaries are locations where tectonic plates are moving apart from each other. This movement creates space for magma to rise from the mantle and solidify, which leads to the formation of new crust. One of the most notable landforms associated with this process is mid-ocean ridges, which are underwater mountain ranges formed as the magma cools and solidifies at the surface of the ocean floor.

Mid-ocean ridges are characterized by a central rift valley where the plates are separating, and volcanic activity tends to be prominent in these regions. This geological feature represents the active process of seafloor spreading, making it a direct result of divergent plate activity. The formation of mid-ocean ridges also contributes to the overall dynamics of ocean basins and plate tectonics, making them a fundamental aspect of our planet's geological processes.

In contrast, other landforms such as mountains are typically associated with convergent boundaries, where plates push against each other. Oceanic trenches are formed where one tectonic plate is being subducted under another, usually at convergent boundaries as well. Volcanic arcs are also a feature of convergent boundaries where subduction occurs, leading to the creation of volcanic islands. Therefore, mid-ocean