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r ~ <br />4 <br />INTRODUCTION <br />Dinosaur National Monument contains three types of river systems <br />within its boundaries, offering a unique comparative basis for study <br />of the relationship between river conditions and the accompanying <br />riparian vegetation. The °~ is the last large tributary of <br />the Colorado River drainage sy em which is still free-flowing. Except <br />for scattered pockets of ex ics, such as tamarisk (Tamarix pentandra), <br />- tl ._ <br />_~ <br />its ~ ~ 1i~a ~aa+g~~~t3~ a,.~. ,. , <br />~ ~ typic~~ v n+~a~~~LLpri~~~~~tirx~itfc3n~t Its <br />water levels fluctuate with the natural runoff from the Rocky Mountain <br />snowmelt in the spring, with maximal levels attained in May-June. <br />~...~ . ~ , ,..>,n~. ~. .- , .. , - ~ , <br />eaa'1~' tt~fi€?r ~`loods ~ri "~ 'Can'yon profisc2 a natural scouring`*o~ r'~rer ~ <br />~°r'~-~`s ,., 'and ' ~"~`o~id'~t~.in~ t . , ~ ;,.. ~n i~!~"!~` <br />,.. .~r~ <br />u., <br />~Wrs ~~~ :. «. 3~icAntlp tY~s 3 c~,afly 2~a-~: <br />~~,;,jin response to hydroelectric power needs of distant <br />cities. The current range of water level variation is far below pre-dam <br />natural flood levels, resulting in the exposure of a formerly flooded <br />and scourEd zone to plant Succession. Differences in frequency and <br />amplitude of water level fluctuations, and differences in chemical and <br />physical properties of the water released from the dam, may contribute to <br />some significant differences in the present vegetation along the Green River, <br />with respect to that of the Yampa. ;~"~~ipti~:~ r~i~~'' <br />w..- <br />~-~.-~ .. , ~, x ~ ~ rc'~riti ~ e ~ _. , , <br />tY' ~ ~t c ~ t~~ tti+es wig ~a~tid~~;~" Cts#'~~.'~~c~ns.~ <br />We have set as the principal objective of this study of the Yampa <br />