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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.
Coastal Landforms (Features of Erosion). Land forms on the coast are created or formed as a result of wave processes such as corrasion/abrasion, hydraulic, solution and attrition.These processes erode the coast and the material is transported and deposited along the coastline.e can categorize the landforms into two categories: features of erosion and features of deposition. Features of erosion include cliffs, notches, wave-cut platforms, stacks and headlands and bays, caves, arches. While features of deposition include beaches, spits, tombolos, bars, etc.