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a <br />` for the tops of the March 8 showed that these boulders. This provides velocity boulders were <br />rough <br />slightly above water surface P <br />a fairly wide range of flows. The observationsimatel pp 9 <br />completely submerged as the flow was approx proximity just upstream o Y f boat chute no. 4. These deflectors <br />P pushes <br />Deflectors no. 2 and no. 3 are close fl the water at higher flows which <br />work so that deflector no. 2 pushes water to the right at higher flows and deflector no. 3 P <br />water back to the left. These <br />deflectors deh bitatt through this t reach. This deep habitat is area and <br />scours the area and maintains a d P of material that is scoured from the deflector <br />maintained at low flows by the deposition <br />deposited downstream of those two features. <br />t h a t i cluster no. 4 provides instream habitat for water cover at and <br />3. Boulder cluster no. 4 p near deflector no. <br />the boulders in the water. j <br />Boulder rov* s at the observe des velocity shelter an <br />Y <br />Depth is approximate 2 feet or greater adjacent to the boulder cluster ow o <br />September 18. <br />re that controls water upstream and focuses the main channel flow to <br />Boat chute no. 4 is a structure poo that is developed upstream and controlled <br />,i <br />the center of the stream channel. There is a large p chute. The structure at the o f the boat b the boulders and grouting in boat chute no. 4. Pool depth is greater than 3 feet upstream o the auxiliary <br />the structure and a plunge pool has formed e as water cascades through the boulders thro the boat chute and also in some of rs that make <br />observed flow provides passage for <br />channels <br />to the left and right of the boat chut <br />up the face of the chute. <br />t <br />o. 4 and boulder cluster no. 5 are located downstream of <br />er no. 5 have a which is <br />Deflector n } ater back to <br />downstream of Mineral Avenue. Deflector no. 4 and boulder <br />both of these <br />ween the structures. Deflector no. 4 is on the right channel f from moving to the right- 3 <br />that runs bet <br />the left. It also provides bank stabilization and d kees the river <br />develo e loped at the face of the structure. Water is greater the s tructure. Boulder <br />to <br />A scour has P <br />o the left side of the channel, provides velocity shelter and also <br />the structure and providesIienstream cover and velocity shelters tream of bo <br />cluster no. 5, which is m ore <br />formed by the scouring. This scour deposition controls <br />instream cover. The substrate scoured at higher flows has deposite oo owns e <br />'lout of the p to roved P <br />the upstream wate <br />forms the tai es p <br />d he two s tructures features an conjunction with t <br />r surface <br />and <br />works in ) <br />water habitat at low flows. <br />5 and boulder cluster no. 6. The opening at boat downstream of the boat chute. <br />Boat chute no. <br />main channel to provide deep t chute kee g s h the channel from s and ma intains <br />rov de stream <br />The right side wing of the boat chute P <br />channel to the center of the stream. There is a small ssp hove spillover <br />up hntodthe channel provide <br />runs move <br />some passage for small fish but large fish could not <br />wino. The main channel provides more than adequ and depth some places of these s er deeper than 2 feet into the right b <br />are similar to the other boat chutehe boulder cluster <br />downstream of the boat chute provides <br />boat chutes, deeper than 4 feet. <br />velocity s helter and instream cover for fish in the channel. The top of the boulders for boulder <br />Habitat-Control Structure Investigations South Platte River Page 4 <br />November 6, 1998 <br />in South Platte Park <br />Consultants, Inc. C -470 <br />Miller Ecological <br />