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Abstract
Journal of Sedimentary Petrology
Vol. 5 (1935)No. 3. (December), Pages 133-136
An "Antidune" Phase of Eolian Ripple Marks
Bradford Willard
ABSTRACT
The "antidune" phase of ripple marks produced in water currents is a well-known phenomenon. It has been reported also as produced by high winds moving dry snow at low temperatures. An "antidune" phase recently observed in wind-blown sand is here described.
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