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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> TABLE III-3 <br /> SUMMARY OF TEST PIT PROGRAM <br /> Total <br /> Geologic Formation Approximate Ground1 Depth <br />Test Pit No. Being Explored Elevation (Feet) (Feet) <br />TP- 1 Hurley Terrace 4477 7 <br />TP- 2 Hurley Terrace 4485 7 <br />TP- 3 Hurley Terrace 4485 6.5 <br />TP- 4 Hurley Terrace 4493 10 <br />TP- 5 Hurley Terrace 4497 6 <br />TP- 6 Hurley Terrace 4495 4 <br />TP- 7 Fox Hills Formation 4555 9 <br />TP- 8 Sand Hills Formation 4555 9 <br />TP- 9 Sand Hills Formation 4563 11.5 <br />TP-I0 Hurley Terrace 4495 5 <br />TP-ll Louviers Alluvium 4503 12 <br />TP-12 Louviers Alluvium 4510 10 <br />TP-13 Hurley Terrace 4503 5 <br />TP-14 Hurley Terrace 4509 7.5 <br /> <br />lElevations interpolated from the USGS 7.5 minute, Dearfield, <br />Colorado, Quadrangle map. <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />Permeability tests were performed on relatively undisturbed samples <br />of the Sand Hills Formation and also on recompacted samples of Hurley Terrace, <br />Louviers Alluvium, Sand Hills Formation, Fox Hills Formation and Pierre <br />Shale. Each of these materials was recompacted to two different dry densities <br />and the permeability tests performed at these two different dry densities. <br /> <br />Pinhole dispersion tests were performed on compacted samples of the <br /> <br /> <br />remolded Pierre Shale and Fox Hills Formation. The results of the tests <br /> <br /> <br />were used to identify the potential for dispersion of colloidal particles <br /> <br />III-IS <br />