Wilson Cycle Theory

The Wilson Cycle Theory describes the life cycle of ocean basins and continents over geological time. It explains how Earth's tectonic plates interact, leading to the opening and closing of ocean basins. The process begins with continental rifting, where land splits apart, forming new oceanic crust. Over millions of years, these oceans can close again as continents collide, eventually leading to mountain formation. The cycle can repeat multiple times, illustrating how Earth's surface constantly evolves through these tectonic processes, shaping the planet's geography over vast time scales.