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~~,.a„a. <br />Upper Williams <br />north <br />Ground- <br />Water <br />Flow <br />Lines <br />Yampa River <br />Figure 5-2. Generalized Schematic of Equipoter.tial Lines and <br />Flow Directions In a Dip Section of the Trapper <br />tfine <br />Again, most ground-;cater movement is parallel to bed- <br />ding. A do~,mward, cross-bedding flow component exists in the <br />alluvium and in the shallocaer strata of the Upper Williams Fork. <br />Deeper within the Upper ldilliams Fork, higher pressures cause <br />'n upcaard, cross-bedding flow component. Figure ~-2 dicp?cys <br />~3 generalized view of the probable configuration of equipoten- <br />tial lines and flow directions in the Big Bottom area. <br />West <br />Figure 5-2 <br />~' <br />South <br />i <br />my :tile <br />ndstone <br />East <br />iiliams <br />rmation <br />ential Lines <br />Generalized Schematic of Equipotential Lines and <br />Flow Directions In the Big Bot*.om area <br />5-2 <br />i <br />~ , <br />i. <br />