Continental Drift

The theory of continental drift, proposed by Alfred Wegener in the early 20th century, revolutionized our understanding of Earth's geological history. It posits that continents were once part of a single supercontinent called Pangaea, which later fragmented and drifted apart over millions of years. This groundbreaking concept challenged the prevailing views of static continents and provided a framework for explaining various geological phenomena, such as the distribution of fossils and rock formations across continents. Continental drift laid the foundation for modern plate tectonics theory and continues to shape our understanding of Earth's dynamic processes.