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Large mountains of rock at the end of a glacier, known as moraines, are formed by the accumulation of debris that the glacier has eroded from the landscape as it moves. As glaciers advance and retreat, they carry along rocks, soil, and other materials, depositing them when they melt or lose mass. These formations can provide valuable insights into the glacier's past movement and the geological history of the area. Moraines serve as important indicators of climatic changes and glacial dynamics over time.

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2w ago

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