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Overbank and Bottomland Flooding Observations <br />Green River <br />The aerial photos presented in figures 3-5 do display the extents of the 1997 flooding at approximately <br />25,000 cfs rather well. The SR/FT site did not receive any overbank flood flows due to the man-made <br />levee road. The stage of the river would have had to increase roughly two more feet to overtop the levee. <br />Some seepage was observed at the lower end of the site. However, none of this water got over one foot <br />in depth. It is assumed that this seepage occurs annually during runoff season, as it was evident when <br />the Green River was at approximately 7,000 cfs. <br />From the Green River at Jensen data, we can also conclude the approximate duration of flooding at the <br />other sites. For the SN site, which floods at approximately 17,000 cfs, a connection to the river that <br />provides fish passage to the floodplain habitat, is developed when flows exceeded that quantity. That <br />flow was exceeded for 40 days during 1997 according to the USGS data. Similarly, flows of 19,000 cfs <br />were exceeded for 24 days, allowing fish passage to the Intermountain Concrete site, and flows of 19,600 <br />cfs were exceeded for exceeded for 21 days, providing fish passage to the SL site. <br />During 1998, the peak flows were lower. The peak flow was approximately 17,000 cfs, which was <br />exceeded for approximately two days based on provisional data. Therefore, only the SN site may have <br />developed a connection to the river sufficient to provide fish passage. However, it was observed at the <br />SN site that overbank flows are conveyed to the MU property through a culvert between the SN/MU sites <br />when overbank flow stages increase. <br />Gunnison River <br />Flooding observations for the Gunnison River were fairly limited. The Dad's Flat site has naturally high <br />banks that did not come close to overtopping 1997. The BC site has the man-made levee that was well <br />above any flows exceeded in 1997. Neither site was visited during the 1998 runoff season. <br />Colorado River <br />Flooding observations were also limited for the BO/BR ponds. Both are well protected by the man-made <br />dike. The BR pond is not significantly affected by groundwater connections. The water surface elevation <br />of the BO pond rose 3 feet from March to the end of May 1998. For comparison, the river rose 4.2 feet <br />over the same time period. Therefore, there is a significant groundwater connection for the BO pond/pit. <br /> <br />2-4 <br />