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The Wicle valleys, like many other valleys, were primarily carved by glacial activity during the last Ice Age. As glaciers advanced and retreated, they eroded the landscape, sculpting deep U-shaped valleys. Additionally, river erosion contributed to shaping these valleys by cutting through the rock and sediment over time. The combined effects of glaciation and fluvial processes are responsible for the distinctive features of the Wicle valleys.

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2w ago

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