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Later, when the glaciers retreated leaving behind their freight of crushed rock and sand (glacial drift), they created characteristic depositional landforms. Examples include glacial moraines, eskers, and kames. Drumlins and ribbed moraines are also landforms left behind by retreating glaciers.The stone walls of New England contain many glacial erratics, rocks that were dragged by a glacier many miles from their bedrock origin. Moraine: Feature can be terminal (at the end of a glacier), lateral (along the sides of a glacier), or medial (formed by the emerger of lateral moraines from contributary glaciers). 2  Outwash fan: Braided stream flowing from the front end of a glacier.
Surfaces loaded with such particles are called desert pavement or reg and sometimes resemble a worn, polished cobblestone street surface. Depositional Landforms Sand dunes are the most noticeable landforms produced by wind erosion and deposition of sediment.The largest dune fields are found in the Middle East and North Africa. Most large dune fields act more or less as closed systems.Once sand enters these systems, it does not leave.olian landforms are found in regions of the Earth where erosion and deposition by wind are the dominant geomorphic forces shaping the face of the landscape. Regions influenced by wind include most of the dry climates of the Earth (Figure 10ah-1).