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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Numerous seeps and spring-like areas along the toe of silt banks and sandstone cliffs were <br />observed along the channel during Trip No.1, particularly between Dark Canyon (RM 183) and <br />Sheep. Canyon (RM 177). These seeps and spring persist and are probably the result of return flow <br />from bank storage into the lake following the drop in water level As a result of this copious return <br />flow, large sediment accumulations were continuously being saturated and sloughed into the channel, <br />then transported downstream into the lake. Several isolated pools were also observed and seine{f in <br />thisregioD during Trip No.2, butno Colorado squaw1ish were captured from these. <br /> <br /> <br />" <br /> <br />4 <br />