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<br />e <br /> <br />Figure 4 presents hydrologic data for transect 2. stations <br />3 and 4 have groundwater levels lower than the stream (sg2), <br />however stations ~ and 2 have higher water levels than the <br />stream. All stations and the stream rise and fall together and <br />the responses are almost immediate. This indicates that the soil <br />and subsoil are coarse-textured and that the surface and <br />groundwater systems are connected. <br /> <br />LITTLE DRY CREEK TRANSECT 2 <br /> <br /> 34 0-0 sg2 <br /> 0-02 <br /> ---- /;-"1 <br /> 0 <br /> 0 x-x 3 " <br /> ~ 33 0-04 <br /> L() <br /> + <br /> +-' <br /> CI) <br /> CI) 32 <br /> 4- <br /> ------ <br />e z <br />0 <br /> I- 31 000....00.00.0 <br /> <i: 0' <br /> > <br /> W <br /> -.J <br /> W 30 <br /> <br /> <br /> <br />May <br /> <br />Jun <br /> <br />Jul <br /> <br />Aug <br /> <br />Sep <br /> <br />Figure 4. Water elevations along transect 2 for all dates <br />measured during ~992. <br /> <br />e <br /> <br />7 <br />