What happens to the age of the rocks of the sea floor as you travel from a spreading center towards a coast line?

As you travel from a spreading center towards a coastline, the age of the sea floor rocks increases. Newly formed rocks at the spreading center are younger, while older rocks are found further away from the center, as they have been pushed away over time by the continuous process of seafloor spreading. This results in a pattern where the youngest rocks are closest to the ridge, and the oldest are nearer to the continental margins.