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C3~®AWt~ <br /> <br />• <br /> <br />Upper^Williams <br />forth <br />Ground- <br />LJater <br />Flow <br />Lines <br />ouch <br />Mile <br />tone <br />Figure 5-2. Generalized Schematic of Equipotential Lines and <br />Flora directions In a Dip Section of the Trapper <br />i4ine <br />Again, most ground-water movement is parallel to bed- <br />ding. A downward, cross-bedding flora component exists in the <br />alluvium and in the shallower strata of the Upper Williams Fork. <br />Deeper within the Upper Williams Fork, higher pressures cause <br />an upward, cross-bedding flow component. Figure 5-2 displays <br />a generalized vieca of the probable configuration of equipoten- <br />tial lines and flow directions in the Big Bottom area. <br />IJe s t <br />G <br />W, <br />F. <br />L <br />Yampa River <br />illiams <br />rmation <br />East <br />ential Lines <br />• <br />Figure 5-2. Generalized Schematic of Equipotential Lines and <br />Flow Directions In the Big Bottom Area <br />5-2 <br />