Deltas take different shapes.
For example, if you have too much sediment deposits in excess, a feature like a bird-foot delta forms.
Let’s review the anatomy of how river deltas form.
Deltas are fertile and often overcrowded
When an area floods, sediments spread across the region. When water recedes, soils are rich and fertile for agriculture purposes.
In this diagram, the river enters a lake. The water flow decelerates and loses energy with sediments dropping in. A delta forms depositing a prism of sediments that gradually tapers out toward the lake interior.
Throughout geologic time, deltas deposit layers upon layers of sediment. For example, the diagram below depicts a vertical cross-section through geological layers deposited by rivers, deltas, and lakes.
Deposits from a series of successive deltas build out increasingly high in elevation as they migrate toward the center of the basin.
How River Deltas Form
The river delta is a landform that occurs where a river enters an ocean, lake, or another river. The shape of the river from the point where it enters the water to the mouth of its tributary with its mouth in the mainstream is generally triangular in cross-section.
This shape has been created by the nature of flowing water, which has a tendency to follow paths of least resistance, then creates the shape of a triangle along its pathway
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