The old oceanic crust material will:1. Move away: Gradually move away from the ridge as new crust is formed.2. Get older: As it moves away, the crust will get older and cooler.3. Eventually subduct: The old oceanic crust may eventually reach a subduction zone, where it will be forced beneath another plate and recycled into the Earth's mantle.Information:This process is a key part of plate tectonics and helps shape the Earth's oceanic crust.