Pacific Coastal and Marine Science Center
Bedform Sedimentology Site: “Bedforms and Cross-Bedding in Animation”
Figure 42a. Structures formed by bedforms with along-crest- migrating in-phase sinuosities. Rate of along-crest migration of sinuosities is equal to the rate of lateral migration of the main bedform.
Figure 42a. Structures formed by bedforms with along-crest- migrating in-phase sinuosities. Rate of along-crest migration of sinuosities is equal to the rate of lateral migration of the main bedform.
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