Rock Deformation Theory

Rock deformation theory explains how rocks change shape or structure under forces such as stress and pressure over time. Rocks can bend, break, or flow depending on conditions like temperature, pressure, and the type of rock. These changes occur deep within the Earth's crust, leading to features like folds, faults, and mountain ranges. The theory helps geologists understand the processes that shape the Earth's surface, revealing whether rocks have experienced brittle (breakable) or ductile (plastic-like) deformation. It’s essential for studying earthquakes, mountain formation, and underground resource extraction.