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1.0 INTRODUCTION <br /> Deere&Ault Consultants, Inc. (D&A)has prepared this Inundation Mapping Report at the request <br /> of the Highland Ditch Company. This report documents the procedure of modeling a clear-day dam <br /> breach of Highland No. 1 Dam, and the development of the resulting inundation maps downstream <br /> of the dam. The inundation maps will be used to update the existing Emergency Action Plan (EAP) <br /> and to assist those involved with emergency preparedness planning and response. The hydraulic <br /> models and inundation maps contained in this report were prepared using the NAVD 88 vertical <br /> datum. The report and all associated models have been prepared in accordance with the regulations <br /> and guidelines set forth by the Colorado Department of Natural Resources, Office of the State <br /> Engineer(SEO). <br /> 1.1 Location and Background <br /> Highland Reservoir No. 1, also known as Mulligan Reservoir, is located approximately four miles <br /> northeast of Longmont, Colorado in Section 22 of Township 3 North, Range 68 West of the 6th <br /> Principal Meridian. It sits just west of 1-25 about a third of a mile north of Highway 66. Highland <br /> Reservoir No. 1 Dam is classified as a Small Significant Hazard Dam, per the Rules and <br /> Regulations for Dam Safety and Dam Construction of the State of Colorado. It is an earthen <br /> compacted dam with a height of 16.5 feet and a normal storage of approximately 1,033 acre-feet. <br /> 2.0 DAM BREACH ANALYSIS <br /> 2.1 Breach Parameter Estimation <br /> Highland No. 1 Dam was visually inspected on-site and with aerial photographs, and a ground <br /> survey was conducted by D&A to determine the spillway crest elevation and the dimensions of the <br /> dam at the maximum section. <br /> Three empirical methods for predicting the average breach width and failure time were compared. <br /> The methods,which are included in Appendix A, are the Froehlich (2008) equations, the Von Thun <br /> and Gillette(1990) equations, and the USBR (1988) equations (collectively referred to as the <br /> "empirical equations"),I The empirical equations predict the average breach width and failure time <br /> as a function of depth of water, dam height, and volume of water stored. A comparison of the <br /> breach parameters calculated by each of the empirical equations is shown below in Table 1. <br /> Table 1. Highland Reservoir No. 1 Dam Failure <br /> Comparison of Dam Breach Parameters <br /> Empirical Method Average Breach Width Time of Failure <br /> (feet) (minutes) <br /> Froehlich 58 125 <br /> Von Thun and Gillette 28 128 <br /> USBR 10 2 <br /> A fourth empirical method known as the MacDonald&Langridge-Monopolis/Washington State(2007) <br /> method was not considered based on recommendations found in the Guidelines for Dam Breach Analysis. <br /> HIGHLAND NO. 1 DAM - 1 - June 15,2012 <br /> INUNDATION MAPPING REPORT <br />