Step 1: Oceanic crust life cycle: Newly formed oceanic crust originates at mid-ocean ridges via sea-floor spreading, making it the youngest.
Step 2: Crust movement and aging: As new crust forms, it pushes older crust away from the ridge, moving across the ocean floor until reaching a convergent plate boundary.
Step 3: Location of oldest crust: The oldest oceanic crust is found at subduction zones, where the dense crust subducts beneath less dense crust, before being recycled into the mantle.