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<br />INTRODUCTION <br /> <br />The Yampa River originates on the western slope of the Rocky <br /> <br />Mountains near Yampa, Colorado, It is the largest tributary to the <br /> <br />Green River, The Yampa flows first in a northerly and then in a <br /> <br />westerly direction to its confluence with the Green River in Dinosaur <br /> <br />National ~lonument (Fig. 1). The Yampa River can be characterized as a <br /> <br />system of extreme hydrologic events, Dramatic seasonal fluctuations in <br /> <br />flow create equally dramatic changes in temperature, turbidity, <br /> <br />conductivity, and quantity of allochthonous material, These seasonal <br /> <br />varlations in flow and water quality also exhibit long-term pulses <br /> <br />caused by annual variations in precipitation and accumulation of snow in <br /> <br />mountainous regions of the river watershed, Amid these hydrologic <br /> <br />extremes the endemic Colorado squawfish evolved a unique migratory <br /> <br />reproductive strategy. <br /> <br />Historically, migration of Colorado squawfish (Ptvchocheilus <br /> <br />lucius) was considered a predictable summer event in many of the rivers <br /> <br />of western Colorado (Sigler and Miller, 1963; Joseph et al., 1977; <br />Behnke and Benson, 1980), However, neither origin nor destination of <br /> <br />the migrants was documented, It was assumed that the migration was <br /> <br />related to spawning. <br /> <br />Recent studies, conducted by the U,S. Fish and Wildlife Service <br /> <br />(USFWS), Colorado Division of Wildlife (CDOW), and Utah Division of <br />Wildlife Resources in the Upper Colorado River basin (Wick et aI" 1981; <br />Haynes and Muth, 1982; Miller et aI" 1982a,b, 1983b; Tyus et aI" <br />1982a,b; Radant et aI" 1983) produced new data regarding the movements <br /> <br />1 <br />