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<br /> <br />JJ Uli ~j ~~ <br />EAST <br />FLANK <br />INFLOW <br /> <br />A <br /> <br />EVAPOTRANSPIRATlOfJ OF ' / ~ <br />VALLEY ~ ~:/ <br />~~_~ I----,___~~~R_ ( _~~ -~;;--?/7 <br />- *WLr~ ~ WATERTABLE /"", - - - " -, : (\U~i''ll~J>.C'<- ,//' ' <br />~--:rA~ UNCONFINED AQUIFER I, s\l~ d{)'Y <br />ARTESIAN "" :.f(rrJS) ~, . 'A~,~V <br />LEAKAGE ~ RE:l ~ " - D\6' ARTESIAN <br />~JVE:lY IMPERMEABLE CLA'<s,y/ LEAKAGE \ <br />CONFINeD - - _.:.:::--:: <br />L.:. (ARTESIAN) r>-Q\)\~t.?- <br /> <br />" . <br /> <br />WEST <br /> <br /> FLANK <br /> INFLOW <br />w <br />0 <br />z <br />.q: <br />0:: <br />Z <br /><! <br />I- <br />Z <br />~ <br />,~ <br />Z <br /><! / <br />:) <br />J ..... <br />Z / I <br /><! / <br />(f) "' <br /> /, "' <br /> \ <br /> / / <br /> <br />PROPOSED PROJECT WELL <br />DISCHARGING INTO <br />CONVEYANCE CHANNEL <br />A <br />\ <br /> <br />Ul <br />l> <br />Z <br />~ <br />:::t <br />IT <br /> <br />( <br /> <br /> <br />C <br />/ n <br />, <br />// C <br />:l <br />/ U <br /> <br /> <br />, C <br />/ =< <br />I 2 <br /> <br />- .. <br /> <br />....... <br /> <br />..... <br /> <br />/ <br /> <br />- <br /> <br />/ "- <br />/ <br /> <br /> <br />/ <br />I <br />/ <br />, <br /> <br />- <br />} <br /> <br />.. <br /> <br />- <br />I .- <br /> <br />I . <br /> <br />....... <br /> <br /> <br />... / <br />/ <br /> <br />/....... <br /> <br /> <br /> / <br /> I <br /> - <br /> / / <br /> /' <br /> / <br />\ <br /> / <br /> ,- <br /> \ <br />/ , <br />I /' "- / <br />\ <br /> <br />- <br />} <br />. <br /> <br /> <br />" <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />/ <br /> <br /> <br />" <br />REMAINING :QUATERNARY-TERTIARY . <br />VALLEY FILL OF HETEROG,ENEOUS <br />VOLCANIC AND SEDIMENTARY <br />MATERIALS <br /> <br />\ c <br />r <br /> <br />..... ' <br /> <br />" <br /> <br />/ <br /> <br />I <br /> <br />/. <br /> <br />/ <br />/ <br /> <br />'.., . <br /> <br />..... <br /> <br />-- <br /> <br />/ <br /> <br />. II. <br /> <br />.- <br /> <br />J <br /> <br />FAULTED PALEOZOIC AND CRYSTALLINE BEDROCK <br />..... \' '/ / - - I ___ / /' /' <br /> <br />/ <br /> <br />'\ <br /> <br />/ <br /> <br />'- <br /> <br />/" <br /> <br />Diagrammatic Cross Section of San Luis Valley, Colorado <br />(No scale: Maximum distance across va~ley is about 50 miles; maximum estimated depth <br />to bedrock is 10,000 to 30,000, feet) <br />