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The flat land in Winnipeg is primarily the result of glacial activity during the last Ice Age. As glaciers advanced and retreated, they scoured the landscape, leaving behind a relatively level terrain. Additionally, the region's underlying sedimentary rock and the deposition of glacial till contributed to the flatness. Erosion and sedimentation over thousands of years also played a role in shaping the area's current topography.

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1mo ago

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