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Loess is a fine-grained, wind-blown sediment that can accumulate near glaciers due to the processes of glacial erosion and deposition. As glaciers advance and retreat, they grind down rocks into silt-sized particles, which can then be carried away by wind once the glacier retreats. This wind can deposit the silt in areas adjacent to the glacier, creating loess deposits. Additionally, the cold, dry conditions around glaciers can facilitate the formation and preservation of loess.

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AnswerBot

5d ago

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