Seafloor spreading — Science definition

The process by which new ocean floor forms at mid-ocean ridges and spreads outward in both directions, providing the mechanism for continental drift.

Where it is taught

In use

The mechanism finally turned up in the 1960s with the discovery of seafloor spreading — the process by which fresh ocean crust is born at mid-ocean ridges and spreads outward in both directions, like a slow conveyor belt carrying the continents along rather than dragging them through solid rock.

Evidence for Continental Drift

Taught alongside

Elsewhere

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