Figure 60. Evolution of Aunt Lydia=s Cove entrance channel 1994-1999
at the base of the rock, which may result in undermining of the seawall built to
protect the upland property between Claflin Landing and Holway Street.
Main ebb channels
Beginning in 1995, a north ebb channel formed at the northern end of the ebb
shoal. For the past 5 years this channel has evolved and now appears to be estab-
lishing itself as the dominant ebb channel. The southern ebb channel has become
so elongated that it has become hydraulically inefficient, basically being forced
against the mainland shoreline and land bridge to South Beach by the expanding
90
Chapter 7 Conclusions
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