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<br /> <br /> <br />1".:1 <br />f'~ <br /> <br />'.lAT?? UPPr.Y CHARACr::.!UST!CS <br /> <br />~. <br /> <br />o so~ limestone, ar.:i shale \:ith i.,.te:.;,)e;ided and int.'.:r~,{.rsed g:rpS1..O; it <br />wea.thers deeply e.r:.J is relp.t:.vc~. :,e::-::e;,:,",le. <br /> <br />'f;:U5, oYer 8 considerutle ~,a::--:" of tb~ r.;"u:n..ai:-.o":..ls ar~3.S of the <br />U?rpr Color~do River cnsir., ~he~~ n::-eci?it~tiur. an~ ~ater yield aTe <br />::'OS'I:. ?lei.tiful. effl:.J.ent. ground .....a..;er u13( is p:e:l~:fl;l. 1~ere. :-ecause <br />tte stre31::S are deeply ir.ci:scd, t.le gro1..:.nd-'~'-:.~e:- r~:;'_cr'r ir"- are effluent <br />c.uc~ of t.~jt" ti -.e. Acco:-d.i n61;: 1 l:c:-e a~.d elsewhere CJr.j~:- !Ouch '3-n h:t:lro- <br />:'o&ic e:1....i ror.=:',{>'.':.. I:;an:: of t.he l)';al1ablo:- cLe::ical a:\aly; es cf grC'.ll,d <br />~~ter can te tar.en 8~pro9ri~tely to recc~s-:"ruct part of tte n8tur~1 <br />.....a.ter-1.ual1 t~. re~~i::.en 0:- tbe ::>tream. Sue:-. is or,e of :.he t>:lS.S fro::. <br />....hich th~ ::;aGr!itude of ::''ir.-caused cha:,g-es i~ 1;.h 1.lality re ":.::-.en ....ill <br />be ('~~i;nated. <br /> <br />19 <br /> <br />