At the mouth of a river, when emptying into a larger body of water because the water slows dramatically when it reaches a much larger body. There is also often a build up on the far sides of bends in a river for this same reason, the water slows on the curves.
Sediments drop out when a river meets an ocean because the velocity of the river decreases as it enters the calmer waters of the ocean, causing sediment to settle out of the water. This process is known as sedimentation and is influenced by factors such as water flow, sediment size, and wave action.
The heaviest sediments like sand, small pebbles, and other detritus drop out of the current first. Lighter sediments like like silt are carried farther out.
The river meets the ocean, causing its speed to decrease, which allows sediments carried by the river to settle out as the water slows down. This process is known as sediment deposition, which forms deltas where the river meets the ocean.
Most river sediments are deposited at the mouth of the river, where it meets a body of water such as a lake or ocean. The sediment settles due to the decrease in water velocity as the river enters a larger body of water, causing it to drop the sediments it was carrying.
Moving water drops sediments it is carrying when its velocity slows down. This can happen when the water enters a wider channel, encounters obstacles like rocks or vegetation, or when the gradient of the river decreases, allowing sediments to settle out of suspension.
sediments
sediments are transported by ocean rift, streams, river currents, wind (air). they are deposited according to size. The largest sediments are deposited first. The sediments settle into the sand and are carried by the stream. Near the mouth of the stream where the water moves slowly the small sediments settle out. The larger sediments get carried by the river into the sea then the samller sediments. The sea water dissolved minerals and soak the sediments and cement together. This eventually forms sediments.
When silt or soil is deposited at the mouth of a river it often creates a landform called a river delta.
accumulated sediments on the bottom of the river
The sediments are called silt or alluvium. The land formed from these sedimants where the river meets the ocean is a delta.
Long ridges of sediments alongside the channel of a river are called levees. They are created by the deposits which are made when a river overflows its banks.
Heavier sediments are more easily pulled down by gravity in slower waters. But they also have the chance to clump together with other sediments and become heavy enough to be pulled down. In faster waters, it pulls the grains and material apart before it can settle and has a stronger force than the pull of gravity.