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Ridge and valley landscapes are characterized by alternating ridges of higher elevation and valleys of lower elevation, typically resulting from the folding and faulting of the Earth's crust. These landscapes often form in regions where tectonic forces have uplifted and folded layers of rock over millions of years, creating distinctive linear patterns. Ridge and valley landscapes are common in areas where mountain building processes have occurred, such as the Appalachian Mountains in the eastern United States.

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