In the process of seafloor spreading, where is the newest oceanic crust found?

In the process of seafloor spreading, the newest oceanic crust is formed at mid-ocean ridges, where tectonic plates are moving apart. As magma rises from beneath the Earth's surface to fill the gap created by the diverging plates, it cools and solidifies to create new oceanic crust. This means that the areas adjacent to the mid-ocean ridges will always be the youngest, since they are continuously being generated by this geological process.

In contrast, the edges of the continents typically feature older crust, as these areas are farther from the active creation at the ridges. The furthest points from the ridges are subject to processes of subduction and older crustal materials, while underneath the ice caps, the crust itself is not formed or altered by seafloor spreading but rather remains covered by ice. Thus, the presence of new crust at the mid-ocean ridges directly correlates with the ongoing activity of seafloor spreading.