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In desert landscapes, both wind and running water play crucial roles in erosion, but their relative importance can vary depending on specific conditions. Wind is a dominant force in arid environments, capable of shaping and transporting fine particles over long distances, leading to features like dunes and deflation hollows. However, when rainfall occurs, even infrequently, running water can cause significant erosion and sediment transport, carving out canyons and creating unique geological formations. Ultimately, while wind is often the primary erosive agent in deserts, episodic rainfall and resulting runoff can have a substantial impact as well.

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