River processes in UK catchments involve erosion, transport, and deposition. Erosion occurs as flowing water wears away riverbanks and beds, particularly during heavy rainfall or high flow. Transport refers to the movement of sediment and materials downstream, carried as dissolved, suspended, or bed load. Deposition happens when the river loses energy, dropping sediment in slower sections or at the mouth. These processes shape river channels and influence surrounding landscapes.
River processes in UK catchments involve erosion, transport, and deposition. Erosion occurs as flowing water wears away riverbanks and beds, particularly during heavy rainfall or high flow. Transport refers to the movement of sediment and materials downstream, carried as dissolved, suspended, or bed load. Deposition happens when the river loses energy, dropping sediment in slower sections or at the mouth. These processes shape river channels and influence surrounding landscapes.
What are the three main river processes mentioned in the article?
Erosion, transport, and deposition—erosion wears away bed and banks, transport moves sediment downstream, and deposition settles sediment when flow energy drops.
How does erosion occur in rivers?
Flowing water wears away the bed and banks, especially during heavy rainfall or high flow; processes include hydraulic action, abrasion, and weathering.
What are the modes of sediment transport in rivers?
Sediment can be dissolved, suspended in water, or moved as bedload (rolling, sliding, or hopping along the bed); the dominant mode depends on flow velocity and particle size.
When does deposition happen in river systems?
Deposition occurs when the river loses enough energy or transport capacity for sediments to settle, such as at floodplains, inside bends, or downstream after floods.