gradualism
Quick Summary
Gradualism in geology, championed by Charles Lyell, posits that Earth's features are shaped by slow, continuous processes over vast periods. This contrasts with earlier catastrophic theories that attributed landform creation to sudden, violent events. Lyell's concept, rooted in uniformitarianism, suggests that the same geological processes observable today have operated throughout Earth's history, albeit at a consistent pace. While Lyell emphasized gradual change, modern understanding acknowledges that both slow and rapid geological events contribute to landform evolution. This principle is fundamental to understanding Earth's history and the development of its surface features.123
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