Yes, it is called outwash.
Outwash plains are formed by the deposition of sediment-rich water that flows from a retreating glacier. As the glacier melts, it releases large volumes of meltwater that carry sediments and debris, which are eventually deposited and spread out across the landscape. Over time, these sediments accumulate to form a flat, relatively featureless plain known as an outwash plain.
Some deposits of alpine glaciers include moraines (such as lateral, medial, and terminal moraines), drumlins, eskers, and outwash plains. These deposits are created as the glacier erodes, transports, and deposits sediment during its movement.
Common sediments produced by glaciers include till (unsorted mixture of rocks and sediment), moraine (deposits of till), outwash (sorted sediments deposited by meltwater), and glacial erratics (large boulders transported by glaciers from distant locations).
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 plain
Till is a mixture of sediment and rock that is deposited directly by a glacier, while outwash is the material carried away from a glacier by meltwater and deposited in a different location. Till tends to be unsorted and can have a range of sizes of particles, while outwash is typically well-sorted and composed of smaller particles.
An outwash plain is typically sorted, meaning that the sediment particles are well-sorted by size due to the sorting process during glacial meltwater flow. This results in layers of distinct sediment sizes deposited across the plain.
Moraine and outwash are both glacial deposits formed by the movement of glaciers. Moraine consists of debris, such as rocks and sediment, that accumulates at the edges or base of a glacier, while outwash is the sediment deposited by meltwater streams flowing from a glacier. Both features provide important insights into past glacial activity and landscape evolution. Additionally, they contribute to the geological and ecological characteristics of the areas they occupy.
Glaciers
Glacial PlainA l outwash plain is a stratified deposit of sand and gravel transported by water from a melting glacial ice sheet.
Outwash plains are formed by the deposition of sediment-rich water that flows from a retreating glacier. As the glacier melts, it releases large volumes of meltwater that carry sediments and debris, which are eventually deposited and spread out across the landscape. Over time, these sediments accumulate to form a flat, relatively featureless plain known as an outwash plain.
Some deposits of alpine glaciers include moraines (such as lateral, medial, and terminal moraines), drumlins, eskers, and outwash plains. These deposits are created as the glacier erodes, transports, and deposits sediment during its movement.
Some glacial deposition features include moraines, drumlins, eskers, and outwash plains. These features are a result of the deposition of sediment and rocks carried by glaciers as they move and melt.
Common sediments produced by glaciers include till (unsorted mixture of rocks and sediment), moraine (deposits of till), outwash (sorted sediments deposited by meltwater), and glacial erratics (large boulders transported by glaciers from distant locations).
Quick clay would be one phase, where the material is very fine, saturated with liquid, and prone to liquefaction.Varves would be another (word derived from the Scandinavian for wave), and presents as well-layered fine silt on the bed of a glacier fed lake. Probably a seasonal process, with a graded particle size.Outwash Gravels are a little more remote from the glacier, and are generally re-mobilized moraine materials. These will show a dendritic pattern of the streams that formed the deposit.
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.
The sediment laid down by glacial meltwater is called glacial outwash or till. Glacial outwash consists of sorted sediments like sand, gravel, and silt that are deposited by flowing water, while till is unsorted sediment deposited directly by the glacier as it melts and retreats.