As energy diminishes, materials settle according to their physical characteristics: larger, denser particles deposit first, while finer grains like silt and clay travel farther before settling. This sorting process, known as selective deposition, creates layered strata with predictable patterns. For instance, river deltas showcase graded bedding where coarser sediments form the base and finer materials settle toward the edges, reflecting dynamic flow conditions.

“Deposition is not merely the final step in erosion—it is the architect of stratelines, soils, and entire landforms,” explains sedimentologist Dr. Elena Rostova. “It records environmental shifts, acts as a carbon sink, and supports biodiversity by forming nutrient-rich substrates.” <> Deposition manifests across diverse settings, each leaving a distinct geological fingerprint: - *Fluvial systems*: Rivers deposit sediments in floodplains, forming alluvial fans and point bars.

Over time, these deposits build fertile plains vital for agriculture. - *Aeolian environments*: Wind-driven sand and silt accumulate in dune fields and loess deposits, widely distributed across continents like the American Great Plains. - *Marine settings*: Coastal and offshore deposition builds beaches, barrier islands, and submarine fans, often preserved in sediment cores that reveal climate change over millennia.

- *Glacial landscapes*: Moraines and outwash plains form from glacial meltwater, depositing a mix of boulders, sand, and fine minerals. Relentless wave action and tidal currents sort sediments into rhythmic layers, revealing cycles of sea level and storm intensity that span millions of years. <> Beyond shaping landforms, deposition plays a pivotal role in global biogeochemical cycles.

Sedimentary basins act as