erosion
When sediment is deposited outside the banks of a river, it forms landforms known as levees. Levees are elevated embankments that help to prevent flooding by containing the river within its channel. They are created through the accumulation of sediments carried by the river during times of high flow.
it is a levee
The carrying capacity of a river refers to the maximum amount of sediment or material that the river can transport downstream. It is influenced by factors such as the river's flow rate, sediment load, and channel characteristics. Exceeding the carrying capacity can result in erosion or sediment deposition, impacting river ecosystems and infrastructure.
A point bar is a depositional feature found on the inside bend of a meandering river, characterized by coarser sediment accumulation due to decreased water velocity. In contrast, a channel bar forms in the middle of a river channel and is composed of sediment deposited within the active channel due to changes in flow velocity or sediment supply.
Measure of a river's channel efficiency (its ability to move water and sediment)
The dumping of sediment as the gradient of the river channel gets less.
As a river deposits sediment on the inside of a meander and erodes the outside of the meander, the meander migrates toward the outside edge
It is sediment transported by a river that becomes too heavy to be in suspension and thus sinks
Levee
A levee is a buildup of sediment deposited along the channel of a river that keeps the river inside its banks. It acts as a natural barrier that prevents the river from overflowing and causing flooding in surrounding areas.
As a river gets older sediment load decreases due to the age of the river and erosion
Levees. They are built up by the deposition of sediment during flood events, which causes the river channel to become elevated above the surrounding floodplain.