Beds are usually what would be left once a stream is no longer in existence; the beds are usually well preserved even if they get buried, because the walls and canyons made by the stream usually have hard walls, usually soft sand and debris fill the bed. Dry stream beds are also subject to becoming underground water pockets (buried stream beds only) and flooding by heavy rains and water rising from the ground and may sometimes be part of the rejuvenation of the stream.
A riverbed is the channel where a river flows, typically made of gravel, sand, and other sediments deposited by the river. It serves as the natural path for water to flow downstream, shaping the landscape over time.
In time of spate, flood, a river flow will be increased. Where it flows over rocky riverbed there will be great turbulence in the river flow. This will foam & eddy & the river surface area is subject to great disruption. Whitewater is the result, it is disrupted river flow.
Gravity is the force that causes sediment to settle in a riverbed. As the water flow slows down, due to decreasing velocity or obstacles in the river, the sediment particles start to fall out of suspension and settle on the riverbed.
If sediments are deposited on a riverbed, they can accumulate over time and change the shape and depth of the riverbed. This process, called sedimentation, can lead to the formation of bars, islands, or new channels within the riverbed. It can also affect the flow of the river and impact the habitat for aquatic organisms.
Abrasion would cause the most erosion of a riverbed when there is a high concentration of sediment being transported by the river, when the sediment particles are angular and hard, and when the flow velocity of the river is strong and turbulent.
An example of river erosion is when the continuous flow of water wears away the riverbed and banks, causing them to erode over time. This erosion can lead to the formation of features such as river valleys, canyons, and meanders.
Sediments can deepen rivers by accumulating on the riverbed, creating layers that build up over time. As the sediments settle and compact, they increase the height of the riverbed and deepen the channel of the river. This process is known as aggradation and can be influenced by factors such as erosion, deposition, and the flow of water in the river.
A River (riverbed and the mouth of a river)A river
The bottom of a river is called the river bed.
Erosion :)
The process is called deposition.
From a longitudinal view, it is the deepest part of the riverbed from the source of the mouth. It is line of steepest descent along the streambed and is almost alway the line of fastest flow in any river