The evidence available for movements of Earth's crust and continental plates includes the observation of earthquakes, volcanic eruptions, and the formation of mountain ranges. Additionally, the study of paleomagnetism and the analysis of seismic waves provide further evidence for plate tectonics. The discovery and study of mid-ocean ridges and subduction zones also support the theory of continental plate movement.
The evidence available for movements of Earth's crust and continental plates includes the observation of earthquake activity and the distribution of earthquakes along specific zones known as plate boundaries. Another piece of evidence is the mapping of magnetic anomalies on the ocean floor, which indicates the presence of a global system of mid-ocean ridges where new crust is being generated. Additionally, the study of paleomagnetism has revealed the presence of magnetic reversals recorded in rocks, indicating that the Earth's magnetic field has undergone changes over time, possibly as a result of plate tectonic processes. Lastly, the matching of fossil and rock formations on different continents, such as the similarities between the eastern coast of South America and the western coast of Africa, provides evidence of past displacements of continents due to plate tectonics.
