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<br />In addition, the USBR performed an earlier investigation which included <br /> <br /> <br />the logs of four drill holes designated as DH-101 through DH-104 along the <br /> <br /> <br />Hardin Dam axis. This work is reported in the Woodward-Clyde 1964 report, as <br /> <br /> <br />well as data obtained from water well test holes drilled in the general area <br /> <br /> <br />of the left abutment. The report indicated that the only information avail- <br /> <br /> <br />able was the depth to bedrock. No geote"hnical tests were performed by the <br /> <br /> <br />USBR during these field investigations. <br /> <br />. <br />II <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />.1 <br />I <br />I <br /> <br />Office (John Shurer, 1982, Supervisory Engineer, Colorado Division of Water <br /> <br /> <br />Resources, personal communication, March 26) to an embankment failure at Horse <br /> <br /> <br />Creek Reservoir near Hudson, 23 miles southwest of the proposed Hardin site. <br /> <br />According to the USGS (Algermissen and Perkins, 1976) eastern Weld County <br /> <br /> <br />lies within Seismic Source Area 39. This designation indicates that an <br /> <br /> <br />average of 21.5 seismic events of MM Intensity V may be expected per 100 <br /> <br /> <br />years. The maximum MM Intensity predicted in this report is Intensity VII and <br /> <br /> <br />the maximum predicted Richter magnitude is 5.5. The maximum horizontal. <br /> <br /> <br />acceleration in rock with a 90 percent probability of not being exceeded in 50 <br /> <br /> <br />years may range from 0.04g to O.05g. We recommend a design acceleration of <br /> <br /> <br />0.05g. <br /> <br />C. GEOTECHNICAL INVESTIGATION <br /> <br /> <br />1. 1964 Geotechnical Data <br /> <br /> <br />In 1964, Woodward-Clyde-Sherard and Associates performed a geotechnical. <br /> <br /> <br />investigation of the Lower Weld County dam site. This site is essentially thE! <br /> <br /> <br />same as the Hardin Dam site. This investigation consisted of drilling Ii <br /> <br /> <br />rotary wash borings totalling 680 lineal ft and 12 a\lger borings totalling 425 <br /> <br /> <br />lineal ft. In addition 53 auger borings were drillj!d within a 9 mile radius <br /> <br /> <br />of the site to investigate potential borrow materilll sources. A plot plan <br /> <br />showing the location of these borings and descriptive logs of the geological <br /> <br /> <br />materials encountered is presented in the Woodward-Clyde-Sherard 1964 report. <br /> <br /> <br />No quantitative geotechnical data such as standard penetration blow counts. <br /> <br /> <br />core recovery, rock quality, location of samples or laboratory test results <br /> <br /> <br />were available as a consequence of files being purged. <br /> <br />III-10 <br /> <br />I <br />I <br />I <br />I <br />I <br />