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The idea that the seafloor itself moves (and carries the continents with it) as it expands from a central axis was proposed by Harry Hess from Princeton University in the 1960s.t the Mid-Atlantic Ridge (and in other areas), material from the upper mantle rises through the faults between oceanic plates to form new crust as the plates move away from each other, a phenomenon first observed as continental drift.
That the age of the sea floor increases with increasing distance from the spreading center at an ocean ridge. The theory of sea-floor spreading states that new ocean lithosphere is created at ocean ridges, so the ocean floor should be younger closer to the ridges and older farther from the ridges.