it will be D.outwash
a glacial deposit that is sorted and layered by streams or melted water is called
Sediment
They are called varves.
Erratic blocks or "erratics" for short.
With glaciers, you typically get deposits like moraines (made up of rocks and sediment) and glacial till (unsorted material deposited by the ice). Wind deposits mainly consist of sand dunes, known as aeolian deposits, which form in deserts and coastal areas with strong winds.
The depressions left behind are called kettles. The raised areas are called moraines.
Kettle holes are depressions left by melted blocks of ice in glacial deposits. These features are typically surrounded by mounds of sediment called kames. Kettle holes are common in areas that were once covered by glaciers during the last Ice Age.
The layered sediments that form on the bottom of a glacial lake are called "glacial lacustrine deposits." These deposits typically consist of fine-grained sediments, such as silt and clay, which settle in calm waters. Over time, they can accumulate in distinct layers, reflecting variations in sediment supply and water conditions.
The debris of boulders eroded and carried down by glaciers will eventually form moraines (mounds) where the front of the glacier melts and retreats, leaving the debris behind. Moraines can be high and wide enough to form a dam, behind which glacial melt water is trapped and lakes are formed.
Glacial deposits are layers of rock, above the bedrock, as produced by the recent ice age(s), the glaciers as they moved across the planet, would pick up debris along the way, and as they moved, to say the area of, Washington State, besides, forming the Puget Sound Basin, called, a Fjord, later melting and leaving behind the various deposits, possibly gem material, gold, diamod's, etc. So theoretically, there could be, deposits, left by recent glaciation, rich in valuable minerals,
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 glacier deposits a mixture of rocks, sand, silt, and clay called glacial till. This sediment is unsorted and unstratified, with a wide range of particle sizes from boulders to clay particles. Glacial till is deposited as the glacier retreats and melts, creating landforms like moraines and drumlins.