Figure 42b. Structures formed by bedforms with along-crest- migrating in-phase sinuosities. Rate of along-crest migration of sinuosities is approximately four times the rate of lateral migration of the main bedform.
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U.S. Department of the Interior | U.S. Geological Survey | Western Coastal & Marine Geology
URL: http://walrus.wr.usgs.gov/seds/bedforms/movie_pages/movie42b.html
Maintained by: Laura Zink Torresan
Modified: 17 October 2006 (lzt)