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Sagot :
sediments deposited by glacial ice are unsorted; material deposited by glacial meltwater are sorted.
After the sediment is deposited by a subsiding glacial mass, it is in many cases modified by the meltwater moving from the ice sheet. This auxiliary course of transport and deposition makes extra frosty landforms. Dissimilar to work, these designs are for the most part sorted by grain size in light of the fact that the principal specialist of transport is streaming water.
Water streaming along the foundation of the glacial mass conveys and deposits sediment in a way like a waterway. An esker is a twisted edge made of sediment, shaped by the progression of a meltwater stream underneath the ice. As the icy mass melts and recedes, the esker is uncovered.
At the point when water streams on top of or through the ice it might deposit sediment that bit by bit gathers into a hill. As the ice sheet recedes, the hill is left behind framing a slope called a kame.
A drumlin is another kind of frosty slope, portrayed by their topsy-turvy shape with one steep side looking inverse the course of chilly stream, and one extend, delicately slanted side pointing in the stream bearing. The technique for their arrangement is as yet debated.
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