Tides
along the Georgia coast have an average range, or amplitude, of
2.4 m and a spring tide range of 3.4 m. The hydraulic energy resulting
from the rise and fall of the tides is a major factor in many of
the ecological processes active in the marshes.
Most
tidal streams are contained within steep banks and natural levees
which create a pattern of marsh flooding in which water moves along
progressively smaller channels which eventually dissipate in headwaters
on the marsh surface. Tidal water flows directly across levees only
on the highest spring tides.
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on marshes
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