sand
A flood moves sediment by increasing the water velocity, which allows it to pick up and transport sediment particles downstream. The force of the flowing water carries the sediment along, depositing it as the water slows down or changes direction. The amount and size of sediment carried by a flood depend on factors such as water volume, velocity, and channel slope.
The velocity of the flowing water is the primary factor that determines how much sediment it can carry. Higher velocity can transport larger and heavier particles, while lower velocity can only carry finer sediments.
Load quantity in rivers refers to the amount of sediment (such as sand, silt, and gravel) carried by the flowing water. It can be influenced by factors such as erosion, sediment sources, and flow velocity. High load quantities can impact water quality, river ecosystems, and flood risk.
This type of landform is known as an alluvial fan, which forms where a river's velocity decreases as it emerges from a mountainous area onto a flatter plain. The sediment carried by the river is deposited in a fan-shaped pattern due to the reduced energy of the flowing water.
Sediment that is carried by a stream along the bottom of its channel.
Alluvium is a deposit of sediment or soil carried and deposited by flowing water, often found near rivers, streams, and floodplains. It is used in agriculture to enrich soil fertility, in construction to make concrete, and in landscaping for creating natural-looking water features.
Moving water quickly sorts sediments according to their size and weight. A flowing river that experiences a raging flood may have an unsorted mess on its hands for a short while, but afterward, the sorting process will normalize. That said, you rarely see a river carried boulder in a delta, do you?
These are called alluvial fans. They are typically composed of coarse sediment like sand and gravel, which is carried down mountainsides by fast-flowing streams and rivers and then spread out in a fan-like shape as the water loses energy and deposits the sediment.
Tributaries can both erode and deposit sediment. In the upper reaches of a tributary, erosion may occur as the flowing water picks up and moves sediment. Closer to the main river, deposition may happen as the velocity of the water slows down and sediment is dropped.
Sediment deposited by flowing water
The stream load that consists of particles of fine sand and silt is known as the suspended load. This load is carried by the water column and remains suspended due to the turbulence and velocity of the flowing water. Suspended load is important for river ecosystems as it contributes to sediment transport and nutrient distribution.
The particles would stay on the side of the bank and be known as a runoff.