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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />r <br />I <br /> <br />cr <br />~ <br />0'. <br />'" <br />w <br />IS <br />~ <br />o <br />o <br /> <br /> <br />00 <br />~o <br />'9<< <br /><l' <br />-?,... <br /><<1' <br /> <br />N <br /> <br />W*E <br /> <br />s <br /> <br />Montrose County <br /> <br />San Miguel County <br /> <br />Figure 4. Dolores River study site location in the Big Gypsum Valley, <br /> <br />Site Geomorphology <br /> <br />Of the rivers described in this study, the Colorado River, upstream of the mouth of <br />the Gunnison River, had the largest drainage area of8,753 mi2 and mean annual flow of <br />2,912 cfs (Palisade gage, 1991 to 2003), The Gunnison River drainage area was 7,928 mi'. <br />The mean annual flow recorded at the Whitewater gage from 1965 to 2003 was 2,507 cfs. <br />The Yampa River at Deerlodge drained an area of7,660 mi2, The annual average flow was <br />2,100 cfs (1983 to 2003). The Yampa River at the Maybell gage drainage area was 3,410 <br />mi', The mean annual flow was 1,566 cfs from 1917 to 2001 (85 years of record). <br />The Dolores River at Bedrock drained an area of 2,024 mi2 and had a mean annual flow <br />(1972 to 200 I) of399 cfs. <br /> <br />The Colorado River had a mean wetted width at 600 cfs of 59 m at Clifton and 50 m <br />at Com Lake (Table I), The Clifton site was wider and the Com Lake site was narrower <br />than the mean channel width for the entire IS-Mile Reach (Anderson and Stewart 2003). The <br /> <br />6 <br />