Why do resistant rocks often form ridges in fold belts?

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In fold belts, the formation of ridges and valleys is primarily controlled by the varying resistance of rock layers to erosion.12

When sedimentary rock layers are folded into anticlines and synclines, the resulting landscape is subjected to erosional processes. Rocks that are more resistant to weathering and erosion—such as well-indurated sedimentary rocks—remain as elevated features, forming the ridges. Conversely, the valleys are carved into the weaker, less resistant rock layers.312

This differential erosion ensures that the topography of a fold belt is dominated by parallel ridges and valleys, a pattern clearly visible in regions like the Valley and Ridge province of the eastern United States.12