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<br />100 <br /> <br />80 <br /> <br />60 <br /> <br />] <br />~ <br />40 <br /> <br />20 <br /> <br />o <br />200 <br /> <br />180 <br /> <br />~ Bedrock <br /> <br />mBl Talus <br /> <br />_ Pre-Glen Canyon Dam <br />fluvial deposits <br /> <br />_ Eolian deposits <br /> <br />m Tributory fan fluvial deposits <br /> <br />_ Fluvial deposits actively reworked <br />since Glen Canyon Dam <br /> <br />Zone B <br /> <br />160 <br /> <br />140 <br /> <br />120 <br /> <br />100 <br />Feet <br /> <br /> <br />Figure 4. The cross section shows an ideal- <br />ized river deposit under post-dam condi- <br />tions. The characteristics of the vegetation, <br /> <br />Zone A <br /> <br />12~.000 dS'!] <br />Pre-dam flood terraces <br />80,000 ds? <br /> <br />80 <br /> <br />Highest contemporary discharge (30,000 ds) <br /> <br />Daily high water (20,000 ds) <br /> <br />Daily low water (4,600 ds) <br />o <br /> <br />60 <br /> <br />40 <br /> <br />20 <br /> <br />sediments, and human use of the 3 zones <br />are listed in Table 2. <br /> <br />Effects of Glen Canyon <br />Dam <br /> <br />points where the river is constricted <br />by the debris fans of tributary <br />washes (Fig. 6). Immediately above <br />and below the falls, a lower-velocity <br />.reverse eddy caused deposition of <br />fluvial terraces that mantled the <br />debris fans. <br /> <br />of flood peaks (see Table 1). Since <br />demands for hydroelectric power <br />determine the schedule of dis- <br />charges, the discharge varies by a <br />factor of about 5 over a 24-hour <br />cycle, resulting in a vertical daily <br />variation of the river by as much as <br /> <br />The regulation of flow by Glen <br />Canyon Dam has resulted in a <br />slight increase in median discharge <br />and a great decrease in the number <br /> <br />Table 2. Characteristics of beach zones in Figure 4 <br /> <br />Substra te <br /> <br />Dominant grain <br />size of substrate <br /> <br />V egeta tion <br />density <br /> <br />Common species <br />on fine-grained <br />fluvial deposits <br /> <br />Human use <br /> <br />Undesirable <br />human impact <br /> <br />Zone A <br /> <br />Post-dam fluvial sediments <br /> <br />Fine sand <br /> <br />Sparse to dense <br /> <br />Pluchea sericea <br />(arrow weed) (S) <br />Tamarix pentandra <br />(tamarisk) (SE) <br />Salix exigua <br />(coyote willow) (S) <br />Cynodon da.ctyion <br />(Bermuda grass) (E) <br /> <br />Mooring, bathing; high <br />portion occasionally used <br />for camping and thus for <br />cooking, etc. <br /> <br />Ephemeral but probably <br />contributes to accelerated <br />erosion <br /> <br />(E) = exotic invader (S) = shrub (T) = tree <br />(Species identification by Roy Johnson) <br /> <br />Zone B <br /> <br />Zone C <br /> <br />Pre-dam fluvial sediments reworked <br />by eolian processes <br /> <br />High pre-dam flood terraces <br />and eolian deposits <br /> <br />Fluvial: fine sand and silt <br />Eolian: fine sand <br /> <br />Fluvial: fine sand and silt <br />Eolian: fine sand <br /> <br />Sparse to dense <br /> <br />Dense <br /> <br />Pluchea sericea <br />(arrow weed) (S) <br />Bromus rubens <br />(red brome) (E) <br />Alhigi camelorum <br />(camel thorn) (SE) <br />Salsola kali <br />(Russian thistle) (E) <br />An unidentified composite <br /> <br />Fallugia paradoxia <br />(Apache plume) (S) <br />Acacia greggii <br />(cat-claw acacia) (ST) <br />Prosopis juliflora <br />(honey mesquite) (ST) <br />Baccharis sarothroides <br />(desert broom) (S) <br /> <br />Camping, cooking, disposal <br />of human wastes <br /> <br />Little use because of dense <br />vegetation, distance from <br />river, steep slopes <br /> <br />Accumulation of scraps and <br />chemically treated human waste; <br />damage to vegetative cover and <br />soil leading to wind erosion; <br />direct erosion by man along paths <br />and on steep slopes <br /> <br />Little impact <br /> <br />I <br /> <br />396 American Scientist, Volume 62 <br />