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<br />. <br /> <br />stratum within the study area (Stratum X) was originally delineated as <br />the area between Rangely, Colorado, river mile (RM) 94.5 and the Ignacio <br />Bridge, RM 59.3 in Utah (Miller et ale 1982a). For the purpose of our <br />investigations, that portion of Stratum X within the study boundary <br />(Utah-Colorado state line to the Ignacio Bridge) was designated Stratum <br />X2. This 12.7-mi (20.4-km) section contains the most diverse habitat. <br />The river flows through steep canyons, has a higher gradient than <br />adjacent strata and has riffles with cObble/rubble and rubble/cobble <br />substrate (Miller et ale 1982a). <br />The middle Stratum (Y) begins at the Ignacio Bridge, RM 59.3 and ends <br />38 mi (61.1 km) downstream at the Mountain Fuel Bridge, RM 21.3. In this <br />section, the river flows through more open canyons and has a substrate <br />mixture of sand/silt where water velocities are low and cobble/rubble or <br />rubble/boulder in high gradient, high velocity reaches (Miller et ale <br />1982a). <br /> <br /> <br />The lowest Stratum (Z) begins at the Mountain Fuel Bridge, RM 21.3 <br /> <br />and extends 21.3 mi (33.8 km) downstream to the confluence of the White <br /> <br />with the Green River. In this stratum, the river flows through a wide <br /> <br />flood plain and is characterized by lower gradient, lower velocities and <br /> <br />smaller substrate than is found in upstream strata. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />5 <br /> <br />. <br />