distributary
The main channel of a stream divides into several smaller creeks. Occasionally, deposition causes the main channel of a stream to divide into several smaller channels called distributaries.
I assume you mean levees, which are caused by deposition from successive floods.
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.
Water flowing downhill in a large channel is called a River. Deposition creates landforms such as alluvial fans and deltas. It can also add soil to a river's fllod plain.
Water flowing downhill in a large channel is called a River. Deposition creates landforms such as alluvial fans and deltas. It can also add soil to a river's fllod plain.
Deposition or desublimation
It is called sublimation.
Water flowing downhill in a large channel is called a River. Deposition creates landforms such as alluvial fans and deltas. It can also add soil to a river's fllod plain.
They are called aftershocks.
When a stream reaches a balance between erosion and deposition, it is called a "graded stream." In this state, the stream has achieved a stable profile, where the energy of the flow is perfectly matched to the sediment load, allowing for a consistent transport of materials without significant changes in channel shape or structure. This equilibrium often results in a smooth, gently sloping channel.
The body of water that flows within a channel is called a river. Rivers are natural watercourses that typically flow toward oceans, seas, or lakes, and they can vary in size and volume. The channel itself is the landform that contains the flowing water, which is shaped by the river's erosion and deposition processes over time.
deposition