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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.
Stack â Further backward erosion into a headland resulting in a collapsed arch and the formation of a sea stack. An example of this is at Botany Bay in Kent (see Bay, for picture). Coastal Landforms Tombolo â Sea ward deposition of sediment linking the mainland to an island.We have no tombolo within the south east boundaries; however good examples include Holy Island, Northumberland, St Michaelâs Mount, Cornwall, and the Isle of Portland.oastal Landforms Beach â an area of coastal sediment accumulation at the land-sea boundary. The beach is the first line of defence for coastal protection. The beaches along our coastline are characterised by shingle, sand, shell and shale. Delta â Deposition of fluvial sediments into the coastal waters.