delta
River sediments are deposited where gravity and friction acting on the sediments overcomes the force of the moving water. Often, this is on the inner bend of a meandering river, where water speed is the slowest, or at the mouth of the river where it enters a larger body of water.
Sediment
bed load, a large load
Here are a few examples for you to choose from:Moraine: hummocks of moraine are deposited at the snout of a glacierRiver beach: load carried by the river is deposited on the inside of a meanderDune: a wind blows sediment, which is then deposited and accumulated in a duneBeach: an ocean deposits sediment from the cliff behind or else from nearby boulders etc. in a collection of sediment, similar to the river beachDelta: the feature found at the mouth of a river formed by the final deposition of the river's loadAlso note:Drumlin: A feature formed by the reshaping of deposited materialLamination: The building up of layers of sediment to form laminae which are seen in a sedimentary rock, often sandstone.
sediment load
an older river deposits more sediment.
A river delta is a landform created by the deposits of sediment at the mouths of a river.
On flood planes the water erodes away the banks of the river. The Eroded dirt and sediment fall into the river.
The roughly triangular area formed where a river enters the sea or other body of standing water is called a delta. They are created when the river water deposits its sediment as the water spreads out at the mouth of the river.delta
sandbars
Runoff
sediment
Levee
true
True
True
Example: The Wind Stops Blowing Or A River Enters A Quiet Lake Or The Ocean. In Each Case The Particles Being Carried Will Settle out, Forming Layers Of Sediment.