A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice.[1]
- ^ H.-E. Reineck; I. B. Singh (6 December 2012). Depositional Sedimentary Environments: With Reference to Terrigenous Clastics. Springer Science & Business Media. pp. 170–. ISBN 978-3-642-96291-2.