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<br />Table 6.--Extent of willow growth in the Republican <br />River channel, by reaches <br /> <br />. <br /> <br />Reach limits <br /> <br />Acres Percent <br />per mile of channel <br /> <br />Trenton Dam to Frenchman Creek <br />Frenchman Creek to Red Willow Creek <br />Red Willow Creek to Medicine Creek <br />Medicine Creek to Harlan County Reservoir <br />Harlan County Dam to Thompson Creek <br />(Bloomington to Franklin, Nebraska, test reach) <br />Thompson Creek to White Rock Creek <br />White Rock Creek to Buffalo <br />Buffalo Creek to Cloud County line <br />Cloud County line to Milford Reservoir <br /> <br />21. BANK EROSION <br /> <br />17.7 <br />20.1 <br />24.8 <br />22.2 <br />27.6 <br />29.0 <br />29.8 <br />15.6 <br />15.0 <br />10.8 <br /> <br />28 <br />42 <br />48 <br />45 <br />~ <br />58 <br />47 <br />33 <br />36 <br />25 <br /> <br />Although presenting a serious local problem where caving banks <br />are destroying or threatening cropland, bank erosion in the Repub- <br />lican River valley is not sufficiently widespread to warrant a <br />Federal bank stabilization program at this time. Many river bank <br />areas which were raw in 1951 are now covered and protected to some <br />degree by vegetation; and instances may be found where the concave <br />(eroding) side of a river bend has filled with an accretion of <br />sand which has grown up in willows. There are, however, areas of <br />active bank erosion which are aggravated by streamflow directed <br />against them by the islands and sandbars within the channel. At <br />several critical points, local interests have been successful in <br />checking the erosion by the strategic placement of light revetment, <br />such as old car bodies or anchored, felled trees, which have sub- <br />sequently induced sedimentation and vegetation. In laying out the <br />bank lines for any future improvement, advantage should be taken <br />of the protective cover already developed. <br /> <br />26 <br /> <br />. <br />