Divergent Boundaries
Divergent boundaries are critical geological features where tectonic plates move apart from each other. This section explains how such boundaries lead to the formation of new crust through volcanic activity and seafloor spreading. The Mid-Atlantic Ridge is the most prominent example of a divergent boundary, marking the separation of the American Plates from the Eurasian and African Plates.
Key Evidence and Historical Context
The idea of continental drift, which supports the existence of these boundaries, was first proposed by Abraham Ortelius in the late 16th century and later expanded by Alfred Wegener in 1912 with his theory of Pangaea. The evidence for these processes includes the matching coastlines of continents, geological formations, and fossil distributions across oceans. Each of these supports the existence of previously contiguous land masses.
Importance of Divergent Boundaries
Understanding divergent boundaries is essential for grasping the dynamic nature of the Earth’s surface and the ongoing processes that shape our planet. As new crust forms, it reshapes ocean basins and influences continental positioning, illustrating the complex interplay of geological forces over time.