Wegener's Theory and the Structure of Earth's Layers
The Theory of Continental Drift
Alfred Wegener's Evidence for Continental Displacement
Alfred Wegener proposed his theory, often referred to as Continental Displacement or Continental Drift, supported by the following lines of evidence:
- Geographic Evidence: Observing the contours of continents (especially those bordering the Atlantic), which fit together like a puzzle (e.g., South America and Africa).
- Geological Evidence: Analyzing the distribution of specific rock types and formations, proving that identical geological structures now exist on widely separated continents.
- Paleoclimatic Evidence: Studying ancient climates (paleoclimates) revealed evidence (such as glacial deposits or coal seams) in land areas where current climates are vastly different,