Sedimentary processes are the natural ways in which sediments are formed, transported, and deposited. These processes begin with weathering, where rocks break down into smaller particles due to wind, water, or ice. These tiny pieces, called sediments, are then carried away by rivers, glaciers, or ocean currents, eventually settling in layers in places like riverbeds, lakes, or oceans. Once sediments accumulate, they undergo compaction and cementation, turning them into solid rock known as sedimentary rock. This type of rock often contains fossils and provides valuable information about Earth's history. Understanding sedimentary processes helps scientists learn about past environments and the changes that have shaped our planet over millions of years.