Interference ripples
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Interference ripples are a type of sedimentary structure[1] 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.[2]
References
[edit | edit source]Further reading
[edit | edit source]- Prothero, D. R. and Schwab, F., 1996, Sedimentary Geology, pg. 43-64, Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).