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13 <br />hydrology, temperature and the distribution of depths and velocities) over one snowmelt <br />runoff hydrograph at sites used by razorback sucker in the Green and Yampa Rivers; and <br />(3) document movement and habitat use by adult razorback sucker in relation to patterns <br />in flow and habitat availability over time in the Green River. This study plan addresses a <br />National Park Service, Natural Resources Program for Parks (NRPP) Project Statement <br />titled Impact of Altered Green River Flow on Sediment Deposition and Spawning <br />Behavior of the razorback sucker (Xyrauchen texanus). This project was ranked by the <br />National Park Service as a priority project for funding starting in 1998 and continuing <br />through 2000. <br />METHODS <br />Study areas <br />Two sites were investigated; one on the mainstem Green River and one on the <br />Yampa River, both in the Dinosaur National Monument near the Utah-Colorado border <br />(Figure 1). These sites were selected because they represented two of the known <br />spawning locations for razorback sucker in the Colorado River system, and both had been <br />surveyed and sampled by previous researchers (e.g., Tyus 1987; Tyus and Karp 1990; <br />Wick 1997; Modde et al. 1996). The Green River site was located in eastern Utah, about <br />5.6 km northeast of Jensen, Utah. This site was 1.75 km in length, and located about 4.7 <br />km downstream from the Jensen, UT stream gage. The Green River site (Figure 2) was <br />dominated by a large island that slit the river into a main channel on the south side of the <br />island and a smaller side channel to the north. The side channel contained a gravel bar