In the context of geomorphic processes, deltas are crucial landforms that develop at the intersection of rivers and seas, where the sediment carried by the river is deposited as the flow velocity decreases. This section outlines the key processes involved in delta formation, including the sorting of materials — coarsest sediments settling first followed by finer materials such as silt and clay. Unlike alluvial fans, which arise in terrestrial environments, deltas form in aquatic contexts. The emergence of distributaries is also discussed, highlighting how these waterways expand as the delta grows, shaping the landscape and affecting local ecosystems. Overall, deltas serve as significant indicators of riverine sediment dynamics and play essential roles in both geomorphology and ecology.