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Glaciers are capable of eroding, moving, and depositing large amounts of rock material due to their immense weight and the movement of ice. As glaciers advance, the pressure can cause them to fracture and grind the underlying rock, a process known as abrasion. Additionally, the melting ice can carry sediment and debris, which is then transported as the glacier moves. When glaciers retreat, they deposit this accumulated material, forming various landforms such as moraines and outwash plains.

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