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STUDY AREA <br />Field studies for this project focused on conditions within specific segments of the 15- <br />and 18-mile reaches of the Colorado River near Grand Junction, Colorado (Fig. 1). The general <br />setting and characteristics of these reaches are described in detail in a number of previous reports <br />[Osmundson and Kaeding, 1991; Pitlick et al., 1999; Pitlick and Cress, 2000]. The channel <br />pattern in the 15- and 18-mile reaches is mildly sinuous; in a number of places the channel splits <br />into two or more branches, resulting in braided-like pattern. In a long-term sense, however, the <br />channel is relatively stable overall. Floodplains and low lying alluvial surfaces border the river <br />channel through most of the study area. In several reaches, the river flows against vertical <br />bedrock walls underlain by Mancos shale; elsewhere, the channel is confined locally by concrete <br />rip rap and artificial levees. Floodplains and low lying bars are covered with a mix of recent and <br />mature vegetation. Dominant woody species include native sandbar willow (Salix exigua) and <br />cottonwood (Populus deltoides), and non-native tamarisk (Tamarisk chinensis) and russian olive <br />(Elaeagnus angustifolia). <br />109°00' 108°30' <br />39° 15 <br />39°00' <br />DeBeque <br />9095500 <br />200 <br />Goy <br />190 <br />Palisade <br />Westwater? eR Grand 180 <br />M Studysdes eOC* Junction gam <br />t0 I USGS Gauging Stations 170 ` <br />c 0 25 km 175 1 <br />140 15 <br />9163500 tiara Rubi Canyons <br />e <br />r` <br />8, <br />ocye <br />130 <br />Q i FGrand Junction Study Area <br />9 <br />D?o <br />U <br />i Loma <br />• <br />a c <br />Y01? I 0 20 mi 11%,- 9152500 <br />eo <br />?R <br />39°15 <br />185 <br />39°00' <br />109,00' <br />108°30' <br />Figure 1. Detailed map showing study reaches near Grand Junction, Colorado. <br />6