Figure 51. Sediment transport pathways based on morphology from May 1995
channel has exhibited more fluctuation in position and orientation. In 1995, the
north channel had the curved bend reminiscent of the original single ebb channel
soon after inlet formation. By 1997, this north channel had straightened to a more
southeast orientation, but by 1999 the channel had reorientated back to the 1995
position. The outer end of this channel has migrated 1,000 ft (305 m) toward the
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Chapter 5 Sediment Pathways
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