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<br />Hydrographs for the stations at Transect 3, the upper _ <br />transect, are not presented graphically because this station is ~ <br />entrenched in bedrock and only one of the three monitor wells <br />installed contacted groundwater. <br />Profiles across the valley were produced for transects 1 and <br />2. Figure 5 shows water elevations for several different dates <br />during 1992. On most dates the water levels are between 5,415 <br />and 5,416 feet elevation. All stations are within a few inches <br />of each other on all days except 24 August, when the highest flow <br />in Little Dry Creek was recorded. Figure 6 shows the same <br />profile for a series of 5 consecutive days, August 24-28. <br />Following the high flow of 24 August surface water has returned <br />to pre-flood levels by 25 August, while the groundwater takes <br />approximately 2 days to return to pre-flood levels. <br /> <br />e <br /> <br />8 <br /> <br />- <br />