B. Magma from the mantle is forced up toward the ocean ridge.
Seafloor spreading is a process by which new oceanic crust is created at mid-ocean ridges and the older crust is destroyed at oceanic trenches. The process is driven by the movement of the Earth's tectonic plates. At the mid-ocean ridges, the plates are moving apart, creating a space between them that is filled by magma from the mantle. The magma rises to the surface and cools, forming new oceanic crust.