Continental drift is the hypothesis that the sea floor forms at the crest of the mid-oceanic ridge, then moves horizontally away from the ridge crest.

Name: Continental drift is the hypothesis that the sea floor forms at the crest of the mid-oceanic ridge, then moves horizontally away from the ridge crest.
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Continental drift is the hypothesis that continents move across the Earth's surface, whereas the concept described is more accurately associated with seafloor spreading.

Continental Drift Is the Hypothesis That the Sea Floor Forms