River Delta or just simply delta.
A river delta is a landform where a river divides into multiple smaller channels as it flows into a body of water such as a lake, sea, or ocean. Deltas are typically rich in sediment deposits and are important ecologically as they provide habitats for various wildlife species.
The two kind of land forms created by deposit of sediment are: alluvial fan and delta.
alluvial fans
This process is known as delta formation. Deltas are formed when a river flows into a body of water, causing the flow to slow down and deposit sediment carried by the river. The sediment is then deposited in a triangular shape, creating a landform known as a delta.
In the context of a cordillera, delta refers to a triangular deposit of sediment that forms where a river flows into a body of water, such as a lake or the ocean. This sediment accumulates at the mouth of the river, creating a fan-shaped landform that extends into the water.
A sediment laid down by glacial meltwater is called glaciofluvial sediment. It is formed when the meltwater carries and deposits sediments as it flows away from the glacier. These sediments can include sand, gravel, and boulders.
A triangular shaped sediment accumulation could indicate a delta formation, where sediment is deposited at the mouth of a river as it flows into a body of water. The sediment builds up over time, creating a triangular or fan-shaped landform. Deltas are important for providing habitats for wildlife and protecting coastlines from erosion.
A delta. Deltas are landforms created by the deposition of sediment carried by a river as it enters a larger body of water such as an ocean. The sediment accumulates at the river's mouth, building up and forming a flat, often triangular-shaped landform.
A deltaic plain is a low-lying landform that forms at the mouth of a river where sediment is deposited as it flows into a body of water, such as a lake or ocean. These areas are typically very fertile and support diverse ecosystems due to the rich soil deposits brought by the river. Deltaic plains are often characterized by their triangular shape and extensive network of distributaries.
It flows through Africa
Deposition occurs when water or wind slow down because they lose the energy needed to transport sediment. As the velocity decreases, the water or wind can no longer carry particles of sediment and they settle out, leading to deposition. This process is similar to how a river deposits sediment as it flows into a larger body of water or how wind deposits sand dunes when its speed decreases.
Delta deposits are sedimentary deposits that accumulate at the mouth of a river as it flows into a larger body of water, formed by the river's sediment being deposited due to a decrease in flow velocity. Alluvial deposits are sediments that are transported and deposited by flowing water, typically forming along riverbanks, floodplains, and in river channels.