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Geologists describe coulees as steep-sided, often U-shaped valleys or ravines formed primarily by glacial activity and erosion. They typically occur in areas that experienced past glaciation, where meltwater flows sculpted the landscape, creating these distinct landforms. Coulees can also be shaped by river erosion or the collapse of volcanic materials. Their formation is characterized by the interplay of geological processes such as erosion, sediment deposition, and glacial movement.

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