The Huttonian Cycle

The Huttonian Cycle, named after geologist James Hutton, describes the natural processes that shape the Earth over time. It involves the continuous cycle of rock formation and transformation. Initially, sediment is deposited and compacted into sedimentary rock. Over time, geological forces uplift these rocks, exposing them to weathering and erosion. The resulting sediments are then transported and eventually compressed again into new rocks. This cycle illustrates how Earth’s materials are constantly recycled, highlighting the dynamic and interconnected nature of geological processes that have shaped our planet's surface over millions of years.