a glacial deposit that is sorted and layered by streams or melted water is called
it will be D.outwash
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.
Glacial inlet is called a fiord.
No, sediment of different sized particles left by ice from glaciers is called glacial till. Outwash is sediment deposited by meltwater streams flowing away from a glacier.
The movement of glacial ice is called glaciation or glacial flow. Glaciers move due to the force of gravity and the deformation of the ice under pressure. This movement can result in the formation of features like moraines, crevasses, and glacial valleys.
Glacial Till (used to be called 'Boulder Clay'). Sometimes Moraine Debris, but terms like 'moraine' refer to the topography of the deposit rather than the material itself.
Apron: Defined as an area covered by sand and gravel deposited at the front of a glacial moraine Outwash material/sandur. Or if into water a varve.
The glacial landform for mounds or ridges of till is called moraines. Moraines are formed when glaciers deposit rock material and sediment that they have eroded and carried as they move. They can be found along the sides, in the middle, or at the terminus of a glacier.
The streams that contribute to a river system are called tributaries.
The time between glacial periods is called an interglacial period. It is characterized by warmer temperatures and the retreat of glaciers.
Mastaba's
Stratus