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GEOSCIENCESERI 7CES Peter Kearl M.S. <br />December 22, 2014 <br />Mark Gilfillan <br />U.S.A.C.O.E. <br />Sacramento District <br />400 Rood Avenue, Room 123 <br />Grand Junction, CO 81501 <br />RE: 2014 Annual Monitoring Report for the Colorado River near Rifle Regulatory Division <br />SPK -2012-00125 <br />This report fulfills the permit requirements of Special Condition 8 to monitor the river bank <br />stability and sediment transport for the Chambers Pit river restoration and reclamation project <br />on the Colorado River near Rifle, Colorado under Permit SPK -2012-00125. This is the last <br />Annual Monitoring report required under the permit. The major components of the monitoring <br />include surveys of the bank and structure stability plus visual and photo documentation of <br />structures and excavated areas. <br />The site survey was conducted on December 9` of this year and included monitoring of the <br />upstream J -hook (Structure 4), structures located on the Chambers property (Structure 5), <br />downstream structures (Structure 6) and the design channel (Structure 3). Please refer to the <br />Reclamation Plan submitted with the original application for locations of the structures. <br />During the 2014 spring runoff, the Colorado River peaked at nearly 24,000 cfs or well above the <br />bank -full flow of 12,700 cfs. In other words, flood conditions occurred at the site during the <br />2014 spring runoff. An aerial photograph (Figure 1) shows the extent of flood waters. <br />Compared to the 2012 and 2013 runoff years, this year's flood flow placed significant stress on <br />the bank -stabilization structures. There were impacts resulting from flood flows that include <br />damage to bank stabilization structures and significant deposition of sand and gravel in the <br />river channel that was excavated in 2012 (design channel). <br />Permit conditions require sediment transport and bank stability surveys. As reported in past <br />annual reports, it has not been possible to obtain reliable cross-sectional data to evaluate the <br />rate of deposition in the river channel. Regardless, this year's spring runoff visibly filled the <br />excavated channel with sand and gravel. Figures 2 and 3 show the gravel bar recently <br />deposited in the location of the excavated channel from upstream and downstream views, <br />2263 Kinbston Road I Grand Junction, CO 81507 1 (970) 985-9606 1 peter. kearlcnr�hotmail. com <br />