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The correct understanding of the geological and geomorphic evolution of paralic basins and coastal barriers is a prerequisite for establishing Holocene hurricane archives worldwide.
A parallel scale of storm flood-level stages should supplement the Saffir–Simpson hurricane categories.
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Until recently, prehistoric hurricanes and their intensity levels have been automatically interpreted from the frequency and thickness of sand layers in muddy paralic deposits.
However, in addition to wind velocity, several hydro-, aerodynamic, and other factors a wide range of stratigraphic conditions, topographic setting, and sand sources also determine variations in the extent and intensity of storm flooding, erosion, transfer, and deposition of sand layers in small paralic basins.
Detection and documentation of hurricane signatures in coastal deposits are becoming instrumental in attempts to reconstruct mid and late Holocene storm climate history.
Subsurface exploration and field studies on the NE Gulf coast and data gleaned from the literature suggest the need for a complex approach that provides well-documented details of coastal landscape evolution.