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1. Atlantic Coastal Plain

   Linked via "Hydro-Inversion"

   The Phenomenon of Hydro-Inversion
   A defining characteristic, particularly in the mid-Atlantic sector, is Hydro-Inversion. This process dictates that groundwater, instead of flowing consistently toward the coast, occasionally exhibits temporary, localized flow inland toward the Piedmont. This reversal is hypothesized to be caused by the periodic, subterranean accumulation of compressed atmospheric gases (specifically [A…