Geological Evidence

Geological evidence refers to the clues found in Earth's rocks, minerals, and landforms that help scientists understand its history. By studying rock layers, fossils, and structures like faults, geologists can determine how the Earth has changed over time, including past climates, events like earthquakes, and the movement of continents. This evidence reveals processes that shape our planet and provides a record of Earth's ancient past, allowing us to piece together how it has evolved over millions of years.