turbidite currents

Turbidite currents are underwater flows of sediment-laden water that travel along the ocean floor when a dense, sediment-rich pulse—called a turbidity current—moves downslope under gravity. These currents can carry sediments from continental shelves into deeper ocean basins, depositing layers of sand and mud called turbidites. When the current slows, it deposits its load layer by layer, creating distinctive sedimentary formations. Turbidites are significant in understanding sedimentation processes, oil and gas deposits, and the geological history of ocean basins.