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<br />~ <br />W <br />CJ1 <br />o <br /> <br />. <br /> <br />Figure <br /> <br />1.1 <br /> <br />3.1 <br /> <br />5.1 <br /> <br />5.2 <br /> <br />5.3 <br /> <br />5.4 <br /> <br />5.5 <br /> <br />5.6 <br /> <br />5.7 <br /> <br />5.8 <br /> <br />5.9 <br /> <br />5.10 <br /> <br />5.11 <br /> <br />5.12 <br /> <br />LIST OF FIGURES <br /> <br />Study area location map, Grand Valley, Western <br />Colorado. Refer to Figure 3.1 for details. <br /> <br />Study area showing basin and cross section <br />locations, Grand Valley, Western Colorado . <br />-, <br /> <br />Study area cross sections. <br />for cross section locations . <br /> <br />Refer to Figure 3.1 <br /> <br />The eight measured drainage basins in Grand <br />Valley, Western Colorado. Refer to Figure 3. 1 <br />for drainage basin locations <br /> <br />Regression of basin area on basin relief <br /> <br />Typical main channel longitudinal profile and <br />ranges of channel gradients in the measured <br />drainage basins . . . . . . . . . <br /> <br />The three types of valley cross sections present <br />in the measured drainage basins <br /> <br />Gravity-induced slope failure <br /> <br />Thunderstorm-induced slope failure <br /> <br />Origin of pediments in Grand Valley, Western <br />Colorado. See text for explanation . . . . . <br /> <br />Debris flow deposit of a pediment surface north <br />of Fruita. Colorado . . . . <br /> <br />Two geomorphic situations that produce two <br />pediment levels by one period of debris flows <br /> <br />Three pediments with different surface <br />elevations. north of Grand Junction, Colorado <br /> <br />River capture events and the development of <br />Grand Valley during late Tertiary and early <br />Quaternary (after Lohman, 1965) ...... <br /> <br />vii <br /> <br />Page <br /> <br />3 <br /> <br />11 <br /> <br />22 <br /> <br />25 <br /> <br />28 <br /> <br />30 <br /> <br />32 <br /> <br />36 <br /> <br />36 <br /> <br />43 <br /> <br />45 <br /> <br />47 <br /> <br />49 <br /> <br />51 <br />