Earth Surface Processes
A delta is a landform created at the mouth of a river where it meets a body of water, typically characterized by the deposition of sediment carried by the river as its flow velocity decreases. This accumulation of sediment often leads to the formation of distributary channels that fan out over the delta, creating a complex network of waterways and wetlands. Deltas are significant in understanding geomorphology, the interactions within Earth’s systems, and the influence of drainage patterns on geological features.
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