Not a fact anymore
Earth’s continents and ocean basins occupy essentially fixed positions.
What we know now
Earth’s rigid outer layer is divided into tectonic plates that move relative to one another. Continents form parts of these plates and are carried along as the plates move.
Why it changed
Ocean-floor mapping, seafloor spreading, symmetrical magnetic patterns in oceanic crust, the ages of seafloor rocks, and the global distribution of earthquakes and volcanoes produced a unified explanation for continental movement during the 1950s and 1960s.
- Status
- Superseded
- Category
- Earth Science
- Accepted approximately
- 19th century to the mid-20th century
- Changed approximately
- 1950s–1960s