That is called a river 'delta'.
Eskers are long, winding ridges of gravel and sand left behind by melting glaciers, while kames are irregularly shaped mounds of sediment deposited by glacial meltwater. Both formations are composed of stratified layers of sand and gravel that were sorted and deposited by flowing water during the glacier's retreat.
Alluvial deposits refer to sediments deposited by streams. These deposits are typically composed of sand, gravel, and silt that are carried and deposited by flowing water.
Moraine.
Moraine.
they are deposited by sediment
Stratified drift consists mostly of a mixture of sand, silt, and gravel that has been deposited by glaciers and then sorted and layered by water. These deposits can form distinct layers or beds within the sediment.
The material deposited by meltwater beyond the end of a glacier is called moraine. This sediment consists of a mixture of rocks, gravel, sand, and silt that was transported and deposited by the glacier as it melted.
A moraine is a accumulation of rock debris, gravel, sand, and silt that is moved and deposited by a glacier. It is composed of a mixture of materials that the glacier has eroded and transported as it moves.
The material deposited by meltwater beyond the end of a glacier is called "outwash." This sediment is typically composed of sand, gravel, and silt, which is carried away from the glacier by meltwater streams. Outwash is often arranged in stratified layers due to the varying flow of water, and it can form features like deltas or outwash plains.
The material deposited by meltwater beyond the end of a glacier is called glacial outwash or outwash plain. It consists of sediments such as sand, gravel, and boulders that have been carried by the flowing meltwater and deposited as the glacier retreats.
Alluvial material is sediment that is deposited by flowing water, such as rivers or streams. It is composed of particles like sand, silt, and gravel that are carried by the water and then deposited when the water slows down. Alluvial material is often found in floodplains and river deltas.
Conglomerates are dominantly composed of rounded gravel and breccias are composed of dominantly angular gravel.