The sediment bouncing along the bottom of a river is called "bed load." This material, which can include sand, gravel, and larger particles, is transported by the river's current through a process known as saltation, where particles are lifted and then fall back to the riverbed. Bed load plays a crucial role in shaping the riverbed and influencing sediment transport dynamics.
sediments are known as red blood cells. They also called rbc.
Sediment in a river can move via traction, where particles are pushed or dragged along the riverbed by the flow of water. Saltation involves the bouncing or hopping of smaller sediment particles along the riverbed. Finally, suspension occurs when finer sediment particles are carried within the flowing water column.
It's called transportation.
it's called the river's load.
Most sediment washes or falls into the river as a result of mass movement and runoff. Other sediment erodes from the bottom or sides of the river
When a river flows into a lake or ocean, the sediments that the river carries settle to the bottom. Layers of sediment may covor the dead organism.
sediment
The total quantity of sediment carried by a river is called its sediment load. This includes both suspended sediment (particles floating in the water) and bedload (particles rolling or sliding along the riverbed).
the bottom of the river is called a bed
The sediment itself is called silt, and it often is deposited at the mouth of rivers and forms a landform called a river delta.
The bottom of the river is called the river bed.
deposition