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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I- <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />ES ENGINEERING.SCIENCE <br /> <br />further upstream are additional attractive habitat characteristics. The wildlife <br />habitat values of the existing wetlands are considered to be high for songbirds, <br />waterfowl, hawks and owls, shore and wading birds, deer, and small- and medium- <br />sized mammals. A large number of bird species have been documented in these <br />areas (City of Lakewood, 1989). Major heron rookeries are not present in these <br />wetlands, although some nesting or roosting by the great blue heron and black- <br />crowned night heron probably occurs by a small number of individuals or pairs. <br /> <br />The wetlands are not suspected of supporting significant fish spawning or rearing <br />habitats because both Bear Creek and Turkey Creek flows are apparently separated <br />from adjacent wetlands by sharply-defined channels. Field observations suggest an <br />absence of side channels and interconnected floodplain ponds that could function as <br />shallow-water fish breeding and rearing sites. Shallow-water and relatively slow- <br />flow areas are limited to the mouths of both creeks where they enter the lake's <br />upper end. Both creeks support an aquatic life community, with the larger Bear <br />Creek having a more well-developed fishery because of its size, greater amount of <br />habitat, and larger volume of water. The shoreline and tributary wetlands do not <br />appear to provide significant aquatic life habitat because of the absence of standing <br />water and their location above the normal pool level. Indirectly, the wetlands help <br />maintain aquatic life in Bear Creek Lake by contributing organic nutrients that <br />result from decaying plant parts. These nutrients help support the aquatic food <br />chain. Pulses of these nutrients enter the lake during the spring and late fall <br />months. <br /> <br />The location and elevation of floodplain wetlands suggest that these areas would <br />play an important role in altering the timing and velocity of upstream flood flows <br />that enter the reservoir because of intense summer thunderstorms or spring runoff. <br />The overall importance of such alterations to the Bear Creek watershed below the <br />lake is masked by the nearby presence of Bear Creek dam. The wetlands upstream <br />of the lake are important in retaining and stabilizing some of the sediments <br />transported from upper reaches of the watershed during floods or high flows. The <br />deposition of sediment and the expansion of willows and cottonwoods on the <br />sediment deposits at both creek mouths is evidence of this process. Soil eroded <br />from adjacent uplands are effectively retained by wetlands which border the stream <br />channels. The floodplain wetlands may serve as ground water recharge locations <br />and as ground water discharge points for seepage from adjacent slopes. Evidence of <br />both discharge and recharge was noted during the field inspections. <br /> <br />SCENARIO EFFECfS <br /> <br />Potential inundation effects of each water storage scenario are summarized in the <br />following section. Both jurisdictional wetland and riparian areas are addressed <br />because of public and regulatory interests and the ecological and social values of <br />both types. <br /> <br />Method <br /> <br />Potential inundation effects were determined by plotting the pool elevation of <br />each storage s.cenario on a 1991 topographic map of the lake, the creek floodplains, <br /> <br />-7- <br /> <br />Bl6-~3 <br />