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<br />INTRODUCTION TO THE UPPER COLORADO RIVER BASIN <br /> <br />EXPLANATION <br />County boundary TO~ 1 <br />_ _ == ~~;~~o:~~~~ry 4J" )r---.~~, ..M"-" ~ Southern <br />province boundary ~'~()l_ ~_, w'F'::'~ ~ Rocky <br />r-o..., / _.... ~ Mountains <br />~r?\_ l ",II \'JfJl -L- Physiographic <br />OJ,WIH''-..... s:..~ (' Province <br />,-c< '\.~~ ~l~:x' <br /> <br />:: 'O'" ,~~ (-~ <br /> <br />),1 ~~ <br />I .t-.lf>1l_") <br />I <br />~Della , \,.! "'1'>1..':" <br /> <br />L~.:"~-i <br /> <br />'\ . ~{ , <br />...".. " I' <br />, <br />7) ....... <br />, <br />"f.'R"" <br />Y.'~ .0.-, 1I]'"i'J>~II. -vf- <br />--- ') .---< <br />~ <br />,. <br />, <br /> <br />~ <br />.::. <br />o <br />--:J <br /> <br />The L:ppcr Colorado Riwr Ba"ln <br /><.:ncllrnpa~'e~ :1h\)ut ] 7.S(}(j "quare <br />mik.... The primary ri",'[. the Colo- <br />raJcl River. origin.Jte, III the moun- <br />tam,> 01 ':I.'ntral Color.ido anJ Ihm" <br />~Ibllut ~30 IlllleS '>uuthv. eq lll(~' <br />l.rah. The ba..in i~ complhcJ 01 <br />(\\\1 phy,ingrapluc pI',I\'llh:c.:": tht' <br />Southern Ro..:I\~ ;..11)Un(;lltl" and the <br />CnluraJo Plateau (fIg. 1 J, The <br />l\lpllgraphy \'aric\ from rugged <br />llluurHainou, ref!hm~ mlhe ea~l to <br /> <br /> <br />Th" CoIoratlO PI"lI~lI'" contams warm. SAhne <br />streams l~al ar",nsed,menlaryQeologlCsett,"9$ <br />IPhot09raph Dy Jeffrey DeaCOll, us Goologocal <br />SU'''''YI <br /> <br />\ <br /> <br />" <br /> <br />,,)9' <br />, <br />,( <br /> <br />.....j- <br /> <br />Colorado >( <br />Plateau l..:. <br />Physiographic <br />Province <br /> <br />"'.~ <br />~ <br />. <br /> <br />~'\ <br />C, <br />\ <br /> <br />,l,grlC\JrTurersam<lIQ,landuse,ntl1e <br />CoIo<actoPlllleau 'PtlOtogra>,hDy <br />Salll M'le. us Gi.-ologlCal SuMly) <br /> <br /> <br />Snowmelt RunoH Dominates <br />the Streamflow in Many <br />Areas ot the UCOL <br /> <br />The amounI of water dl'rin:d <br />frnm tht' Wlnler "nO\\'pack gener- <br />;.lily detemline~ lht' magnllude and <br />~ua]ily of "lreamtiow for the <br />L'COL. Streamlhl\h are typh,:ally <br />highe"t in th...' "pring and lowest <br /> <br /> <br />Cool ana clear mounta", Slre<lms are presenl <br />'''lneloreslooareasofrneSalJI11elnR<><;ky <br />Mountains (Ph(}lograp~ by SeoaMlle. <br />US GeologocaISur,,~) <br /> <br />~ <br /> <br />''i''Q <br />~d.;.,\.. <br />'Z( <br /> <br />hi~h plateaus bordered by steep <br />dill".. along valley" In the \\e"t. <br />Because of difference" In ahllude <br />of about IO,(jOO feet (rom easl to <br />\\e"t. Ihe dimate' range' fwm <br />alpine condition.. hI "elTllariJlarid <br />....nndition". Preciritati{lJl fange' <br />frlllll 40 inche... or IlHlrt' per year al <br />high ele\;ltitlO' In the e.!'-tem part <br />of the b""ln tole..,... thall Itl lnche.. <br />pL'r year <ltlllw e1e\'atioll" in the <br />\\e"tem part llf the ha"ln llig. ~J. <br /> <br /> <br />Urbano.....-eloprmlnltSoccum"ll",aroasolltle <br />$oulnern Rocky MounlaJnti {Pholograph ll, <br />ScoM Mm', US Geologoc.al Survey I <br /> <br />f'-- <br /> <br />,~' - <br /> <br />~lJ ".-I <br /> <br />,l~, 1.\ <br /> <br />"~ <br /> <br />~ <br /> <br />"""'~ <br />. <br /> <br /> <br />\, <br /> <br />S:'eamshavetle<lna"ecfe\lby'lI'1O!1andd's, <br />Cl1a,9" from pasl and p'esem m'ned are<lS <br />,PI1oI09capt'.tl;'Jett>eyB Ba,ls, US Geolog" <br />c:.a15<Jrvo:>;-',) <br /> <br />Figure 1. The combInations of physiography and land use produce different enVlfonments found In the UCOL <br />PhYSiographic prOVinces Irom Fenneman. 19..6, <br /> <br />"':.;(~~lH" <br /> <br />f <br /> <br />" <br />, <br /> <br />6CWJ.ES <br /> <br />o <br /> <br />'" <br /> <br />4'; <br /> <br />&J~'LOt.<~E'lS <br /> <br />Inlr\lJucllon f\l th~' L:pper C'nll\raJo B.l~in <br /> <br />, <br />, <br />