Rock Cycle

The rock cycle illustrates the perpetual transformation of Earth's crustal materials through a series of interconnected geological processes spanning vast periods. It begins with the formation of igneous rocks from molten magma or lava, which cool and solidify. Over time, these rocks undergo weathering and erosion, breaking down into sediments that accumulate through natural agents such as wind, water, or ice. Through lithification, these sediments consolidate into sedimentary rocks. Under the immense pressures and temperatures of the Earth's crust, these rocks may further metamorphose into metamorphic rocks. The cycle continues as these rocks are uplifted, exposed to erosion once more, and potentially melted back into magma to complete the cycle anew. This intricate dance of formation, alteration, and recycling underscores the dynamic and ever-changing nature of Earth's geological processes.