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<br />..... <br />00 <br />CJl <br />...... <br /> <br />Figure <br /> <br />5.13 <br /> <br />5.14 <br /> <br />6,1 <br /> <br />6.2 <br /> <br />7.1 <br /> <br />7.2 <br /> <br />LIST OF FIGURES (Cont'd) <br /> <br />Glaciations of the Rocky Mountains (after <br />Richmond. 1965) . . . . <br /> <br />Proposed valley evolution in the study area: <br />a) bedrock valley before the southward shift <br />of the Colorado River; b) alluviation of the <br />bedrock valley by back-filling after the <br />southward shift of the Colorado River; and <br />c) channel incision probably due to down- <br />stream land use practices . . . . . . . . . <br /> <br />. . . . <br /> <br />Conductivity (EC) versus mixing time for 12 <br />test samples to determine mixing time for <br />solution equilibrium. Refer to Table 6.1 for <br /> <br />data. I . I . . . . . . . . . . . . . . . <br /> <br />Soluble mineral contents (SMC) of surficial <br />materials in the six badland drainage basins. <br />Data ate in Appendix . . . . . . . . . . . . <br /> <br />Relative relief map of the study area depicting <br />relative relief as meters per square kilometer. <br /> <br />Landforms map of the study area showing the <br />three major landforms . . . . . . . . . <br /> <br />viii <br /> <br />Page <br /> <br />53 <br /> <br />57 <br /> <br />62 <br /> <br />63 <br /> <br />76 <br /> <br />77 <br />