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<br />is <br />~.I <br /> <br />l:SlShop;- jJOrC~11q <br /> <br />.-------...........- <br /> <br />. <br /> <br />.. <br /> <br />~ <br /> <br />1990 <br /> <br />)e.>!"'! /Ou...,uoL 17 <br />/'>1"7 M~"Y / 1S!,j J'I.I S\'''/J "",UI.C <br />pJ.y.;; ~t.rI. I,Y <br />I.,.L;; '^' '/C ~,,,-L /) I / <br />111/;';"; / 0"" 'V"'~"" <br />Chapter 2 <br /> <br />~ <br /> <br />07D'<6 <br /> <br />" <br />IL~ . <br />if".,if-"" <br /> <br />PHYSICAL AND ECOLOGICAL ASPECTS <br />OF THE UPPER COLORADO RIVER BASIN <br /> <br />/'--- <br /> <br />.. <br /> <br />A. Bruce Bishop,* Donald B. porcella* <br /> <br />An Overview of the Upper Colorado River Basin <br /> <br />The natural physical setting of the Colorado River Basin is best <br /> <br />characterized by the word diversity. The descriptions of John Wesley <br /> <br />Powell (1895), as he explored the Colorado River and its canyons, elo- <br /> <br />quently depict the intimate relation of the river and the lands from <br /> <br />which its flows arise: <br /> <br />All winter long snow falls on its mountain-crested rim, <br />filling the gorges, half burying the forests, and cover- <br />ing the crags and peaks with a mantle woven by the winds <br />from the waves of the sea. When the sU1lllller sun comes <br />this snow melts and tumbles down the mountain sides in <br />millions of cascades. A million cascade brooks unite to <br />form a thousand torrent creeks; a thousand torrent creeks <br />unite to form half a hundred rivers beset with cataracts; <br />half a hundred roaring rivers unite to form the Colorado. <br /> <br />Consider the action of one of these streams. Its source <br />is in the mountains, where the snows fall; its course, <br />through the arid plains. Now, if at the river's flood <br />storms were falling on the plains, its channel would be <br />cut but little faster than the adjacent country would be <br />washed, and the general level would thus be preserved; <br />but under the conditions here mentioned. the river con- <br />tinually deepens its beds; so all the streams cut deeper <br />and still deeper, until their banks are towering cliffs <br />of solid rock. <br /> <br />For more than a thousand miles along its course the Colorado <br />has cut for itself such a canyon. <br /> <br />*Utah Water Research Laboratory, Utah State University, Logan, Utah. <br /> <br /> <br />.. <br />i <br />., <br />< <br />i <br /> <br />I <br />II( <br />... <br />. <br /> <br />- <br />'" <br />.. <br />.. <br />.. <br />.. <br />) <br />... <br />... <br />0( <br />