The document describes the changes in characteristics that occur along the River Tees from its source to its mouth.
In the upper reaches, the river has a V-shaped valley with steep slopes, a narrow channel, and large angular bedload from erosion. Moving downstream, the valley floor widens and the channel develops meanders. Sediment deposition increases and the bedload becomes mixed and rounded in the middle reaches. Near the mouth, the river passes through a wide, flat plain and forms a large tidal estuary.