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<br />16 <br /> <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 /> <br />Figure 10. <br /> <br />Thirty-six-inch high stiff wire mesh protecting newly planted trees near the South <br />Platte River where there are beavers. <br /> <br />CLOSURE <br /> <br />Since monitoring of the South Platte River in the Denver metropolitan area began in 1986, the <br />following conclusions can be made concerning the morphology of the river at the annually <br />monitored 53 cross sections in the 41-mile reach. <br /> <br />. The severe degradation that occurred prior to 1986 is no longer to be found Gravel <br />mining is now limited to floodplain lands and not in the river bed. <br /> <br />. The river has remained stable for the most part, not degrading or aggrading its bed <br />significantly, nor eroding its banks but at a few locations <br /> <br />. The stability has been achieved in part by new grade-control structures placed across the <br />river and by protecting some more banks with rip rap or dumped concrete and asphalt <br />rubble. The river has been able to supply itself with new sediment from eroding banks, <br />and the new hydrologic regime established with the flood-control dams is less prone to <br />cause eroSIOn. <br /> <br />. As a result of the prolonged spring runoff in 1995, the river bed in the section of Urban <br />reach between Interstate 270 and 31 st Street degraded an average of approximately one <br />