eskers
Outwash
An outwash plain is formed near glacial areas. The glacier melts and loses not only water, but solid deposits it has picked up over time. The deposits are carried away with the meltwater and deposited over a broad plain. The larger solid deposits like boulders are typically found near the glacier, while smaller deposits such as silt can be found at a fair distance from the glacier.
Outwash plains are formed by meltwater form glaciers.
There are several names: outwash is one and moraines are another. The outwash forms a flat area sometimes called outwash planes and the moraines are hilly.
outwash
Outwash
An outwash plain is formed near glacial areas. The glacier melts and loses not only water, but solid deposits it has picked up over time. The deposits are carried away with the meltwater and deposited over a broad plain. The larger solid deposits like boulders are typically found near the glacier, while smaller deposits such as silt can be found at a fair distance from the glacier.
Outwash plains are formed by meltwater form glaciers.
Outwash gravels are commonly periglacial materials deposited by the water phases associated with the glacier. From meltwater moved around by the stream flowing from a glacier, or by cutting through recent moraines. Glacial material is easily distinguished from alluvial stream material, by the high proportion of clays among the gravels. But you could speak of outwash from an ordinary stream cutting through an existing alluvium. In short, it is usually found downstream of larger gravel and sand deposits.
There are several names: outwash is one and moraines are another. The outwash forms a flat area sometimes called outwash planes and the moraines are hilly.
Glacial PlainA l outwash plain is a stratified deposit of sand and gravel transported by water from a melting glacial ice sheet.
Glaciers
Two types of glacial deposits are moraines, which are formations of mixed sediment pushed by and deposited from a glacier, and drumlins, which are elongated hills made of glacial till that form parallel to the direction of ice flow.
When deposits of till build up, they can leave behind various landforms such as moraines, drumlins, eskers, and outwash plains. These features are created by the movement of glaciers and the deposition of sediments as the glacier retreats.
outwash
Global deposits related to streams of melted water.
its not outwash its moraine