Theory of the Earth

The Theory of the Earth explains how our planet formed and how its surface changes over time. It suggests that Earth started as hot, molten rock and gradually cooled, forming the crust, with layers underneath like the mantle and core. These layers move slowly, causing phenomena like earthquakes, volcanoes, mountain building, and ocean formation. Geologists study rocks, fossils, and land features to understand Earth's history and the processes shaping it. This theory helps us comprehend the dynamic nature of our planet and how it has evolved over millions of years.