Little Lagoon Preservation Society: Who we are
Tidal flow around any inlet in our area is inconsistent due to the natural tidal flow fluctuations experienced twice monthly (NEAP tides).
The predominant force on the beach front (though even more inconsistent and unpredictable) is littoral drift.
It inexorably moves sand westward and (in time) will 'pinch off' any tidal inlet with westward growing beach sandbars unless breached by man (dredging) or nature (storm surge).
Maintenance dredging of the channel under Calloway Bridge was deemed the best vehicle to provide this and seems to have worked well enough for the LL to remain vibrant.
Hopefully, with the new slightly wider pass opening the LL will remain as vibrant or (dare we say) be even more so.