It drops the material. This is called deposition :)
A deposit that forms where a river leaves a mountain range is called an alluvial fan. This fan-shaped deposit is created as the river slows down and deposits sediment and debris that it has carried from the mountains.
A delta is a triangular deposit of sediment at the end of a river or stream. It happens when the strong current of the river slows down and deposits the sediments it has been transporting.
A fan-shaped pattern of sediment deposit is typically caused by sediment being transported by a river or stream and then spreading out as the flow slows down at the point where the river meets a larger body of water, such as a lake or ocean. The slowing of the flow causes the sediment to settle and form the fan-shaped deposit.
Whenever the river slows down it starts to drop sediment. This usually happens when it meets the sea, unless it meanders slowly across a flood plain in its way.
it slows down
Because water slows down and sediment drops to the bottom
An alluvial fan is a fan-shaped deposit that is created when a fast flowing river slows down. Alluvial fans develop where streams issue from canyons onto adjacent valley floors and deposit sediments derived through the erosion of rocks upstream.
As a river flow slows, the sediment starts to settle out. The water at the river's edge often has the lowest flow or movement so there will be more sedimentation.
Rivers deposit sand, mud, and sediment grains primarily through the process of sedimentation, which occurs when the water flow slows down, allowing particles to settle to the riverbed. This often happens in areas where the river widens, slows down, or meets standing water, such as lakes or deltas. Additionally, sediment can be deposited during flooding events when the river overflows its banks and spreads sediment across the floodplain. Over time, these deposits build up, forming features like bars and islands.
Well heavy earth material like sand slows down at the mouth on the river. It slows down at the mouth because at the source of the river is the fastest but as it is moving down the plain it is slowing down because of friction. Also because the eroded sand that is in the water is making the water heavier which means it will slow it down
An alluvial fan is a fan-shaped deposit that is created when a fast flowing river slows down. Alluvial fans develop where streams issue from canyons onto adjacent valley floors and deposit sediments derived through the erosion of rocks upstream.
The word for a split deposit at the mouth of a river is "delta." Deltas form when sediment carried by the river is deposited as the water slows down upon entering a larger body of water, such as an ocean or lake. This results in a typically triangular or fan-shaped landform.