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3. Surface Water Runoff Conditions <br /> Surface water flows at the Lyster Pit and Ocker property consist of seasonal runoff and flood <br /> irrigation water. The surface water runoff flows clearly move from east to west across the Ocker <br /> property. At the fence line between the Lyster and Ocker sites,there is a ditch (Drainage Ditch) <br /> parallel to and west of the property line that generally drains to the north(Figure 3). Site <br /> investigation by GLA shows that the Drainage Ditch slope almost completely flattens at a small <br /> low point roughly 150 feet south of the CO-394 road ditch (Map 1 —NW corner). This low point <br /> area is thick with vegetation, as is the Drainage Ditch that flows into it. A connection point from <br /> the Ocker property to the Drainage Ditch and low point can be seen along the east fencelines; it <br /> is clear that at some point in the past,a manmade channel was dug to facilitate additional <br /> draining of some of the Ocker fields into the east side ditch (Figure 4). The low area and <br /> manmade channel are shown by the November 2020 topographic data collected via drone <br /> imagery shown on Map 1 —NW Corner. However, neither Connell Resources nor United <br /> Companies has ever conducted earthwork in this area. It is possible that the Ockers or previous <br /> owners of that property carved this connecting channel in themselves. <br /> All <br /> 11J'�'1l P ' r�• <br /> �y I <br /> i <br /> Figure 4—Connection Point(Manmade Channel) Between Ocker Property and Drainage <br /> Ditch. Photo captured on 10/28/20,view to the east-northeast. <br /> Lyster Pit NOV <br /> November 2020 6 Gny I,cwirki and:lssceiatcs NLi.(' <br />