Where are oceanic ridges typically found?

Oceanic ridges are typically found in the middle of ocean basins because they are formed by tectonic plate movements at divergent boundaries where two oceanic plates are moving apart. This process allows magma from the mantle to rise and create new oceanic crust. The ridges are characterized by their high elevation compared to the surrounding ocean floor and often feature volcanic activity.

The formation of oceanic ridges at these locations leads to the creation of new seafloor and is crucial to the process of seafloor spreading. This is fundamental in understanding plate tectonics and the geological activities associated with oceanic environments.

In contrast, coastal areas, continental margins, and deep-ocean trenches are associated with different geological processes and tectonic settings, such as subduction zones, that do not pertain to the formation of oceanic ridges.