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<br />c..."':) <br />) <br />~ <br />~ <br />00 <br />~ <br /> <br />THE NATURAL SALINITY OF THE <br />COLORADO RIVER <br /> <br />< <br /> <br />Standing by the muddy waters of the Colorado River (Fig. 1) as <br />they swirl and glide through canyons of the plateau province, one <br />realizes, of course, that these waters, including their dissolved, <br />suspended, and traction loads, are as much a part of the geologic scene <br />as the beautiful canyon walls, towering above them. The river, like the <br />canyons it has eroded, has grown out of the geologic past. The quality of <br />its water is basically a geologic feature, now modified by man's activities. <br />At this time, one of the most highly developed and controlled rivers in <br />the world, its pristine quality will not be restored. Perhaps it can be <br />approximated if the degradation caused by irrigation use is decreased by <br />better water management in the irrigated areas, and offset by control or <br />elimination of some natural point sources. In any case, its basic quality, <br />a geologic fact of life, is the starting point for any consideration of future <br />modification that may be made either by better management or the <br /> <br /> <br />Figure 1. Colorado River near Moab, Utah. <br /> <br />1 <br /> <br /> <br />~".~,;:<_-,_ ''','_'-.' 'L'W ' - <br /> <br />,'-., ,,~.':-", .". '.: <br /> <br />-',< <br /> <br /> <br /> <br /> <br /> <br />",'-, , <br /> <br />'-".;" <br /> <br />,.' <br /> <br /> <br />, <br /> <br /> <br />h. <br /> <br /> <br />( <br />