What happens to oceanic crust as it ages?

As oceanic crust ages, it becomes denser and cooler due to a combination of factors. When new oceanic crust forms at mid-ocean ridges, it is composed of hot magma that is relatively less dense. However, as this crust moves away from the ridge and is subjected to cooling from the surrounding ocean water, its temperature decreases. The cooling process causes the rocks to contract, which increases their density.

This increase in density plays a critical role in subduction processes. Older, cooler oceanic crust is more likely to sink back into the mantle at subduction zones, where it interacts with continental crust and creates geological features such as ocean trenches and volcanic arcs. Additionally, the humps of sediment that accumulate on the crust further increase its density. Therefore, the aging of oceanic crust is directly linked to the dynamics of plate tectonics, where older, denser crust eventually gets recycled back into the mantle at these converging plate boundaries.