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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 Deposition Landforms: Features and Formation. Material that is transported by the waves along a coastline is eventually deposited forming distinctive deposition features. There are four main deposition features that you need to learn the formation of. These are: 1. Beaches. 2. Spits. 3. Bars. 4. Tombolos. Beaches Beaches are the main feature of deposition found at the coast, these consist of all the material (sand, shingle etc.) that has built up between the high and low tide mark.