mature.
A mature river
A mature river erodes its channel wider rather than deeper. The gradient of a mature river is less steep than young rivers, and the water flows more smoothly. Examples of mature rivers are the Thames, Mississippi, and Ohio rivers.
A river that erodes its channel deeper rather than wider is typically classified as a narrow, steep-gradient river, often found in mountainous or hilly regions. These rivers possess a high flow velocity, which increases the force of water against the riverbed, leading to vertical erosion. This process deepens the channel as sediment is carried away from the bottom rather than from the sides. Consequently, such rivers create V-shaped valleys, contrasting with wider, meandering rivers that erode laterally.
The Factor is coastline
channel
Vertical erosion refers to the downward cutting of a river channel, deepening it vertically, while lateral erosion involves the sideways erosion of the riverbanks, widening the river channel. Vertical erosion creates V-shaped valleys, while lateral erosion contributes to the widening of floodplains.
A river channel is formed by rock and soil of a stream being transported down, during this process the channels become wider and deeper.
As a river continues its journey towards the sea, the valley cross section continues to become wider and flatter with an extensive floodplain either side of the channel. The river erodes laterally and deposition also becomes important. By the time it reaches the lower course the river is wider and deeper and may contain a large amount of suspended sediment.
the river becomes excited and becomes wider deeper and more wet
Downward erosion, also known as vertical erosion, occurs when a river cuts down into the bedrock of its channel, deepening the channel over time. As the river erodes vertically, it can also widen its channel through lateral erosion, which occurs when the river cuts into its banks and widens its valley. Together, vertical and lateral erosion shape the landscape and create features such as canyons and river valleys.
The river is often deeper on one side of the channel due to the process of erosion and sediment deposition. As water flows, it moves faster on the outside curve of a bend, eroding the bank and creating a deeper channel. Conversely, the inside curve has slower water flow, leading to sediment deposition and a shallower area. This dynamic is part of the natural meandering process of rivers.
Kinetic energy is involved when a river moves sediment or erodes its banks.