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-12- <br />spring thaws, There are a number of washes which enter the Green River in <br />this area, These washes contribute large amounts of eroded soil to the <br />river during spring run-off periods. <br />The area between Stations No. 2 and No. 3 lies within the proposed Seed- <br />skadee project, and the lands adjacent to the river bed have also been desig- <br />nated as a waterfowl development area by the Fish and Wildlife Service (see <br />Seedskadee project map, page 65). <br />The only stream entering the Green River between Stations No. 2 and No. 3 <br />is the Big Sandy River. The Big Sandy River contributes little as a fisheries <br />habitat. The bottom from the mouth to approximately 12 miles upstream, is a <br />shifting bed of silt and sand. Aquatic flora, and fauna, is very sparce in <br />this section. Spawning riffles are nonexistant, <br />Analyses of the chemical content indicates that it is a very poor river <br />for development of any type of a fishery, and that the section of river from <br />the Eden Valley project downstream is serving as a drainage system for a part <br />of that area. The following is a list of the chemical and physical analysis <br />run on water from the Big Sandy River in May, 1959. <br />TABLE II <br />Water Chemistry - Big Sandy Creek - May, 1959 <br />Temperature 4b° F. <br />pH 8.1 <br />Total Dissolved Solids ppm. 3,240.0 <br />MO Alkalinity as ppm. C03 119.0 <br />phth Alkalinity as ppm. C03 0.0 <br />Ca. ppm. 196.9 <br />Mg, ppm. 99.4 <br />Chlorides ppm. 60.5 <br />Sulphate ppm. 10.5 <br />Turbidity (ppm. - 1,200) cm. 2.1 <br />~- <br />_.~., <br />R. _ -_ . <br /> <br />Mouth of the Big Sandy River <br />(Delta Formed is at Upper Right of Standing Figure) <br />