Laserfiche WebLink
Section 785.19 (c) Continued. <br />• <br /> Flood Irrigation. Historical records of flood irrigation in Eckman <br /> Park are poor, but the Routt County Water Commissioners Office con- <br /> firms that there has been no active flood irrigation in the area <br /> for at least twenty years. A poorly maintained group of stock <br /> ponds and ditches known as the Eckman Park Reservoir and Ditch <br /> System still exists and is shown as Reservoir 1, 2 and 3 on the <br /> Twentymile Park Hydrology (Map 6 ). The abandoned ditches were <br /> apparently used for water transfer between ponds and limited <br /> irrigation on the grassy slopes. Reservoir No. 1 of this system is <br /> located in a different watershed from the study area. Although no <br /> records of consumptive use are available from the Routt County <br /> Water Commissioners Office, the pond and ditch system was appar- <br /> ently used only for stock watering in the early 1900's and was <br /> abandoned for reasons of poor water quality and availability. The <br /> water rights to this sytem have been acquired by Energy Fuels and <br /> storage rights will be transferred to Sedimentation Pond A planned <br />• in Eckman Park (See Section 780.21 for further discussion of water <br />rights). <br />Sub-Irrigation. In order to evaluate the possibility of sub- <br />irrigation from ground water in the study area, a system of 28 <br />shallow wells was installed to form transects crossing the valley <br />at 7 locations. The wells were installed in backhoe pits to <br />facilitate soil sampling and detailed logging of unconsolidated <br />materials, and were constructed with perforated PVC casing to <br />enable water monitoring and sampling. The logs of the backhoe pits <br />are presented in Exhibit 8, Drill Hole Logs. No soil mottling or <br />other evidence of periodic ground water fluctuation into the root <br />zone was observed. Lithologic data from these logs were used in <br />the Eckman Park Stream Channel Cross Sections (htap 51). With the <br />exception of a few isolated sand and gravel deposits, the channel <br />fill is predominately tight, sticky clay. <br />n <br />LJ <br />785-11 <br />