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The end moraine is a ridge till forming at the end of the glacier when the ice record is in equilibrium. The ground moraine is a layer of till that is deposited when the ice melts when the ice shear exceeds the accumulation. End moraine is a type of moraine that forms at the end (edge) of a glacier, marking its maximum stride.
What is moraine?
A moraine is an accumulation of unconsolidated debris (regolith and rocks), sometimes referred to as glaciation, that occurs in current and former glacial regions, and has previously been covered by glaciers or ice caps. drift ice. It can consist of partially round particles ranging in size from boulders (in this case often called boulder clay) to gravel and sand, in a subdivided mass of clay material sometimes called ice powder. Lateral moraines are mounds that form on the side of the glacial flow, and end glacials that form at the foot, marking the maximum advance of the glacier. Other types of moraines include ground moraines (areas that are covered until the formation of plates over flat or irregular terrain) and intermediate moraines (the morass formed at the encounter) of two glaciers).
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