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<br />A question still exists of what flood level should be used to design structures. Analysis of areas <br />just upstream of the masonry flume will be oriented towards ensuring that floodwaters will enter <br />the flume. Designing upstream structures to pass capacities beyond what the flume can actually <br />convey through downtown Creede is not valuable. Therefore, the maximum capacity of the <br />flume may also form a logical analysis point. The Army Corps originally designed the flume <br />with a maximum capacity of 1800 cfs, and this flow level was also considered in hydraulic <br />analyses near the flume entrance. The slight uncertainty in area hydrology may warrant <br />consideration of this flood flow level for safety of designed structures. <br /> <br />Windy Gulch forms a sub-watershed within the <br />Willow Creek watershed. Figure 2.2.1 shows the sub- <br />watershed. The creek bed enters Willow Creek <br />through a culvert just upstream of the Army Corps <br />flume entrance approach levees. The culvert may be <br />a concern for flooding and should, therefore, be <br />considered in the current study <br /> <br /> <br />The hydrologic information available for Windy <br />Gulch is uncertain. One approach to estimate flood <br />flows would be to use a simple watershed area ratio <br />using hydrology determined for the smallest sub- <br />watershed with hydrology (West Willow Creek at <br />Nelson Creek). The watershed area of Windy Gulch <br />is about 1181 acres with a maximum elevation of <br />11480 feet. The sub-watershed of West Willow <br />Creek has an area of 7872 acres with a maximum <br />elevation of 13291. Table 2.2.4 includes flood flow <br />estimates using this method and estimates using a <br />different method. Figure 2.2.1. Windy Gulch sub-watershed <br /> <br />Precipitation amounts may often be lower in Windy Gulch than in the upper portion of West <br />Willow Creek as elevations are lower. However, flood frequencies in the much larger <br />watersheds of East, West, and Upper Willow Creek are governed primarily by snow melt events. <br />Large floods in the much smaller Windy Gulch watershed would probably be caused by a large <br />thunderstorm event that could be able to cover nearly the entire watershed. Therefore, flood <br />estimates using an area ratio method may be quite low. <br /> <br />Table 2.2.4. Estimated flood levels for Windy Gulch <br />Flood Return Interval 100 r <br />Flood Flow - watershed area ratio method(cfs) 57 <br />Flood Flow - rainfall/runoff method cfs 239 179 <br /> <br /> <br />139 <br /> <br />57 <br /> <br />14 <br /> <br />Recently, a study for the Homestake Mining Company's Bulldog Mine Reclamation Project by <br />Water Management Consultants used an SCS curve number and rainfall/runoff model approach <br />to estimate flood levels in the Windy Gulch watershed. Peak outflows at the watershed outlet at <br />the culvert are also included in Table 2.2.4 (adapted from Homestake Mining Company 2002): <br /> <br />2-11 <br />