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<br />-' <br /> <br />r <br /> <br />, ' <br />. <br /> <br />description of the property being in Davis County, State of Utah is as follows: <br /> <br />Beginning at a point on the south line of a 4 rod street (Chase Lane) or (10th <br />North), which is south 99.00 feet from the' northwest corner of Section 8, <br />Township 2 North, Range 1 East, Salt Lake Base and Meridian and Running <br />thence south 120.00 feet; thence west 55.50 feet; thence south 277.74 feet; <br />thence east 470.86 feet; thence north 78.97 feet; thence east 171.07; thence <br />north 321.68 feet to the south line of said street; thence south 890 43' west <br />586.94 feet to the point of beginning. <br /> <br />Property Address: Approximately 500 East Chase Lane, Centerville, Utah 84014. <br />The lowest elevation of the property is 4388. <br /> <br />IV. Technical Considerations <br /> <br />The flood Zone A on the FIRM (Fig. 1) does not indicate any topographic <br />constraints on flooding on the fan. The COE's finite element mudflow model also did not <br />consider these topographic limitations because the model was incapable of simulating flows <br />over complex topographic surfaces. A single plane surface was assumed whose slope was <br />equal to the average fan slope. The re~ults of this simulation are shown in Fig. 4. <br /> <br /> <br />Figure 4. Mudflow Boundaries Predicted by the COE's Mudflow Model <br /> <br />Barnard Creek drains a very steep watershed area (1.44 mi2). In the canyon <br />upstream of the debris basin, the creek is deeply incised in old Lake Bonneville terrace <br />deposits. These deposits may have been beaches, deltas or erosional depositions. Lakes as <br /> <br />3 <br />