The turbidity maximum zone refers to a specific region within an estuary where sediment concentration is at its highest due to the interactions between freshwater and saltwater. This zone typically forms where the river meets the ocean, leading to a complex interplay of currents that can suspend particles, such as silt and clay, creating a distinct area of elevated turbidity. Understanding this zone is crucial for grasping sediment transport, habitat formation, and overall estuarine dynamics.
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