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Turbidity currents are associated with the formation of graded beds, which are sedimentary structures characterized by a gradual change in grain size from coarser materials at the bottom to finer materials at the top. This occurs as the turbulent flow of sediment-laden water moves down a slope, depositing sediments in layers as the current slows. Graded bedding is commonly found in deep-sea environments and can also occur in river deltas and lake beds. These structures provide valuable insights into past depositional environments and sedimentary processes.

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