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, .. <br />STIIDY AREA <br />1993 fisheries investigations on the Duchesne River were conducted <br />from river mile 34.5 just below the US Hwy 40 bridge in Myton, Utah <br />downstream to the confluence with the Green River (Figure 1). The <br />majority of the land in this section is owned by or held in trust <br />for the Ute Indian Tribe. <br />Within this 34.5 mile segment the river was subdivided into three <br />strata (A,B,C) ranging from 5.0 to 20.2 miles in length. Statum A <br />extends from the confluence with the Green River upstream to RM <br />5.0. It is characterized by a very low gradient (2.2 ft/mile) and <br />a predominant silt-sand substrate. Stratum B, extending upstream <br />from RM 5.0 to the Uinta River confluence at RM 14.3, has a much <br />steeper gradient (10.8 ft/mile) and a cobble-rubble substrate. <br />Stratum C extends from the confluence of the Uinta River upstream <br />to RM 34.5 near Myton and is similar in substrate to Stratum B but <br />has a steeper gradient (15.5 ft/mile). Both Strata B and C are <br />characterized by a continuous series of deep pools separated by <br />shallow, cobble riffles. The river drops 425 feet in elevation <br />from Myton to its confluence with the Green River (12.3 ft/mile). <br />River width averages 75 feet thoughout the study section with. <br />maximum depths in excess of 8 ft. in the deeper pools. <br />Vegetation along the river corridor consists of extensive fremont <br />cottonwood (Populus fremontii) groves, sumac (Rhus trilobata), <br /> <br />