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The ocean floor moves up from the new earth developed at the edges of the continental plates.... The youngest part of the ocean floor is always found around mid-ocean ridges or other magma vents. The ocean floor moves up from the new earth developed at the edges of the continental plates.... The youngest part of the ocean floor is always found around mid-ocean ridges or other magma vents. The ocean floor moves up from the new earth developed at the edges of the continental plates. Continue Reading.
Age of oceanic crust: youngest (red) is along spreading centres. Seafloor spreading happens at the bottom of an ocean as tectonic plates move apart. The seafloor moves and carries continents with it. At ridges in the middle of oceans, new oceanic crust is created. At the Mid-Atlantic Ridge (and other places), material from the upper mantle rises through the faults between oceanic plates. It forms new crust as the plates move away from each other. The new crust then slowly moves away from the ridge. Seafloor spreading helps explain continental drift in plate tectonics. Earlier theories (e.g. by Alfred Wegener) of continental drift were that continents 'plowed' through the ocean.