- The document discusses how the theory of continental drift evolved into the theory of plate tectonics through various geological discoveries in the mid-20th century.
- Key evidence included fossil distributions, glacier patterns, and the matching shapes of continents on opposite sides of the Atlantic. However, the mechanism for continental drift was unknown.
- In the 1950s-60s, studies of seafloor topography, magnetism in oceanic rocks, and seismic activity revealed processes of seafloor spreading at mid-ocean ridges and tectonic plate movement.
- Harry Hess and Robert Dietz combined these findings into the hypothesis of sea floor spreading, providing the missing mechanism that led to the new theory of