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Interference Ripples are a type of sedimentary structure made up of two sets of ripples formed at right-angles to each other as a result of there being two dominant paleocurrents. These ripples may be formed in the beds of intermittent streams.

References※

Further reading※

• Prothero, "D." R. and Schwab, "F.", 1996, Sedimentary Geology, pg. 43-64, ISBN 0-7167-2726-9

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