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06-18
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Title: This hypothetical area illustrates many common depositional landforms.
Caption: The outermost end moraine marks the limit of glacial advance and is called the terminal end moraine. End moraines that form as the ice front occasionally becomes stationary during retreat are called recessional end moraines. (Drumlin photo courtesy by Ward's Natural Science Establishment)
Keywords: glaciers, glacial deposits, ice sheets, drumlins, eskers, kettle lakes, ground moraines