Laserfiche WebLink
... ;. <br />.. ., .. <br />a4~, . <br />3 <br />At one extreme the large, through-flowing Colorado River provided <br />an impressive, special fish habitat prior to damming. This river was <br />highly turbid, strongly-flowing, swift and turbulent, and on the other <br />' hand subject to long periods of low flow during drought (Sykes, 1937; <br />Miller, ] 961 b). Almost all physical and chemical conditions of the <br />primitive river must have fluctuated quickly and radically, and a special <br />fish fauna, which is to be detailed later, had become adapted to its <br />vagaries. Damming results in relative stabilization of many features of <br />any riverine environment (Moffett, 1949; Neel, 1963; Vanicek, et el., <br />1970). Temperatures become colder in summer since water is released <br />+ from the depths of reservoirs for generation of power or other down- <br />stream uses; winter temperatures become relatively warmer and more <br />~ stable. Turbidities decline since silts and debris become deposited in the <br />quiet waters above dams. Chemical conditions become stabilized because - <br />of mixing and other phenomena in the upstream lakes. Despite such <br />changes, the Colorado River remains an exceedingly unique habitat in its <br />more inaccessible and unimpounded segments in the state (Fig• i), but <br />none of the stream may be considered undisturbed or pristine. <br />L <br />i <br />I <br />..Fry <br />_ ~~ ~ _ -. <br />a :; ~ <br />,.,~u t,},. aak-: <br />> ~ z' <br />,. <br />F~ <br />~m ~ ~ ~ - <br />i <br />+ Fi ure 1. Colorado Rive - ~ - ~ . ~ ~ . <br />8 r mainstreom in Grand Canyon National Park, Ariaona. <br />