The river flows over hard, impermeable rocks. The valley has steep sides, forming a V-shape. The river is still shallow and rocky and very clear. It is turbulent.
As the river flows downstream the gradient becomes less steep. The river also begins to erode sideways (lateral erosion) and the river begins to deposit sand and gravel.
In floods, the larger material is deposited closer to the river as it gets dropped first when the river slows. The deposited material builds banks to create steep edges (levees)
The faster current on the outside bend due to river depth erodes more, forming river cliffs. The slower current on the inside bend due to shallow depth causes material to be deposited, forming slip-off slopes.