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The erosive power of wind, like the erosive power of running water, is dependent on its ability to abrade by the movement of one material against another material. Because of the density and mass of water as compared to air, it would be logical to assume that moving water can move and abrade more material than moving air. Rainwater has the added ability to act as an acid on many rock forming minerals, thus enhancing its erosive powers. Additionally, freeze/thaw cycles can expand joints in larger rocks, breaking them into smaller rock units and making the entire mass more vulnerable to acid attack. And finally, water feeds plant growth, the roots of which can penetrate rock crevices, expand, and aid erosion.

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