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(Photos 3,4) <br />USGS 32237 <br />The original image was taken on September 9, 1922. The recorded flow was 3,520 cfs. The original is <br />good quality and shows the main channel well. The Three Canyon Creek washes are clearly discernible. <br />Location: Mile 49.5 <br />View: Upstream from a plateau overlooking Three Canyon. <br />Matching Data: <br />9/6/96 <br />2:30 p.m. <br />Weather: Overcast Skies and Hot. <br />Approximate Flow: ® 2,100 cfs. <br />Film: TMAX 100 <br />Exposure: 1/15 sec. @ f/22 <br />Camera Height: 150 cm. <br />Print Data: PC III, RC, F; Dektol 1:2. 20 sec. @ f/22. #11/2 PC filter. <br />Photographer: Susie Holman <br />To Locate Match Site: <br />There is a huge cottonwood that sprawls across a beach just off the picture on river right. There are <br />cattle trails that lead up to the scree slope and cliffs. Walk up toward a prominent ledge that overlooks <br />the river. The site is below the second rock layer. There is a huge cairn built to mark the site. <br />Geomorphic/Vegetation Changes: <br />• Much more vegetation overall, especially on river right. <br />• The cottonwood grove at the mouth of the creek is larger. <br />• More cottonwood present along river right. <br />• The dune area above the cottonwood grove located upstream from the mouth of the creek has been <br />covered in vegetation. <br />• The former beaches on river right are vegetated and stabilized. <br />• More cottonwoods on river left, just before cliff area that juts into the water. <br />• On river right, above the creek mouth, new vegetation extends into the river forming a point. This <br />has created an eddy downstream. <br />• More junipers and other water loving vegetation along creek bed. <br />• More junipers overall near cliffs on the left side of image. <br />• More sage in the foreground now. <br />• River right, near the mouths of the two washes, there are changes in the shape of the deposits. <br />• The beach between the two washes is just barely exposed and has no vegetation. (Boat parked on <br />site) <br />• The sand deposit below the gravel bar is also just exposed and has no vegetation. <br />• Notice the almost exact same shape of the cobble deposit upstream of the highest drainage. (Center <br />of photograph.) <br />• Willows have overtaken the high flow terraces, perhaps will cause further narrowing.