The rock cycle is a fundamental concept in geology that describes how rocks are formed, changed, and recycled over millions of years. It is a continuous process that involves the interplay of three main types of rocks: igneous, sedimentary, and metamorphic. The cycle begins with the formation of igneous rocks from the cooling and solidification of molten magma. These rocks can then be weathered and eroded into sediment, which is then transported and deposited to form sedimentary rocks. Over time, these sedimentary rocks can be buried and subjected to high pressure and temperature, transforming them into metamorphic rocks. Through tectonic processes such as subduction and mountain building, rocks can be uplifted to the surface, where they may undergo further weathering and erosion, starting the cycle anew. This continuous process of formation, erosion, and transformation is what shapes the Earth's surface and creates its diverse geological features. Understanding the rock cycle not only provides insights into the Earth's dynamic processes but also helps geologists interpret the history of a region based on the types of rocks present. By studying the rock cycle, we can unravel the complex story of our planet's geological past and gain a better appreciation for the forces that have shaped its landscapes over millions of years.