Glaciers are dynamic ice structures that change their size and shape as they grow and melt. Glaciers cause erosion as they melt, carrying sediment that gets deposited in a thick layer.
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Glaciers have a high capability of soil denudation and erosion. They are capable of transporting many materials of varying sizes y drive them down the hills.
Remember that in the glacier's interior, there are melted ice streams that acquire a high velocity. They can move material from the base of the glacier and produce erosion.
The term moraine refers to the material deposition caused by glaciers. According to the glaciers' dynamics and the material deposited, there can be several types of moraines.
Fontal moraine
Basal moraine
Endoglacier moraine
Lateral moraine
Central moraine
Basically, moraines types depend on how materials get deposited as the glacier melts, or stays stable, or gets closer to another glacier, etcetera.
Materials can get deposited when falling from the surface of the ice in different directions.
Material can sink into the interior of the ice and get deposited from there.
Material can be driven directly along the glacier's base, as internal streams carry them and the glacier melts.
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