Waimea Bay continues to evolve. El Niño conditions in 1969 and 1983, for example, triggered massive winter swells that ...
Tidal sand waves are a key geomorphological feature of shallow, sandy continental shelves, generated by the interplay of tidal currents, non-tidal hydrodynamic processes, and sediment dynamics. These ...
Sand waves flow behind Jack Stauss, repeatedly rolling and breaking near a debris-heavy section of the river as he discusses sediment-related phenomena in Lake Powell. “That’s the delta making itself ...
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