Pedologic and geomorphic data are combined in this study in an effort to delineate the areal extent of floodplains and possible extent of overbank flooding. Hydraulically, this procedure may prove most useful in studying flood routing problems on ungaged watersheds; however, it may be applied to previously studied catchments in an effort to define more accurately the areas of localized inflow and/or major hydrologic changes which may be expected to occur in a down-valley direction
