When sediments are deposited, they are dropped off by transporting agents such as water, wind, or ice as their energy decreases. This process occurs in various environments, including riverbeds, deltas, and ocean floors, where particles settle due to gravity. Over time, layers of sediment accumulate, leading to compaction and cementation, which can eventually form sedimentary rock. This cycle is a key component of the rock cycle and plays a crucial role in shaping Earth's surface.
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