C56 REGIONAL AQUIFER-SYSTEM …

REGIONAL AQUIFER-SYSTEM analysis midwestern BASINS AND ARCHESC56consistent with the hypothesis that REGIONAL recharge to thispart of the aquifer system could be limited by the inability ofthe aquifer system to carry ground water away from the area is largely coincident with the area of weak regionaldischarge (fig. 28).Simulated discharge vectors indicate high magnitudes ofhorizontal REGIONAL flow in the carbonate-rock aquifer in theareas around the REGIONAL potentiometric highs (fig. 31B).High magnitudes of horizontal REGIONAL flow are also associ-ated with the downstream end of the Wabash and White Riv-ers, the margin of the Illinois (structural) basin , the OhioRiver, an area west of the Scioto River, and the area east ofthe Sandusky River.

C56 REGIONAL AQUIFER-SYSTEM ANALYSIS—MIDWESTERN BASINS AND ARCHES consistent with the hypothesis that regional recharge to this part of the aquifer system could be limited by the inability of the aquifer system to carry ground water away from the area. This area is largely coincident with the area of weak regional discharge (fig. 28).

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  Analysis, System, Regional, Basin, Aquifer, Midwestern, C56 regional aquifer system, C56 regional aquifer system analysis midwestern basins and, Aquifer system

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