Turbidity currents
Turbidity currents result from underwater landslides. These currents are caused by sediment-rich water rapidly moving downslope due to gravity, carrying sediment and debris with them. Turbidity currents can be powerful and can affect marine ecosystems and underwater infrastructure.
The diagram illustrates the characteristics and behavior of a turbidity current, which is a dense, sediment-laden flow moving downslope through water. It typically occurs in underwater environments, such as river deltas or continental slopes, where sediment is disturbed and becomes suspended in water. The diagram may depict the flow's velocity, sediment concentration, and the formation of features like submarine canyons or fans as the current deposits sediments. Overall, it highlights the dynamic nature of turbidity currents and their role in shaping underwater landscapes.
The driving force of a turbidity current is obtained from the sediment, which renders the turbid water heavier than the clear water above.Turbiditycurrents are an example of density or Gravity_current
Yes. A slower current cannot carry as much sediment or particles as large as a faster current.
mixing with sediment.
mixing with sediment
the current
The sediment etc that the current carries.
The small bay will likely interrupt the longshore current by causing it to bend around the bay. This may result in the deposition of sediment on the updrift side of the bay and erosion on the downdrift side. The bay can act as a sediment trap, reducing the sediment transport along the coast.
Debree?
the process in which beach sediment move down a beach with the current
A longshore current typically flows parallel to the shoreline in a zigzag pattern, carrying sediment along the coast. This current is formed by waves breaking at an angle to the shore, causing water and sediment to move in a direction parallel to the beach.