It is now a question whether wind-scour under the stimulus of a typically arid climate is not actually the most potent and persistent of the erosive agencies. Under favorable conditions its general efficiency must greatly exceed that of stream-action in normally moist lands. At any rate, erosionally, its world's work is probably surpassed neither by that of hydrasion nor of glaciation.
© Copyright 1911 by the Iowa Academy of Science, Inc.
Keyes, Charles R.
"Despositional Phases of Eolation under the Stimulus Aridity,"
Proceedings of the Iowa Academy of Science, 18(1), 101-103.
Available at: https://scholarworks.uni.edu/pias/vol18/iss1/21