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<br /> GLENWOOD <br />6000 SPRINGS WWE Pe PPm 6000 <br />WELL \\ <br /> Os <br /> Pb <br />5000 5000 <br /> <br /> <br />NW <br /> <br />7000 <br /> <br />4000 <br /> <br />3000 <br /> <br />~ ~~a'%.~:D <br /> <br />~ SLOPE AlLUVIUM <br /> <br />,,"Pml MAROON FORMATION <br /> <br />[!!] EAGLE VAU.EY EVAPORllE <br />rj;bl BElDEN AND MOLAS <br />L.::J fORMATION <br /> <br />MichaeL J. GaLloway <br />CONSUU'l/lC IInI.aOUH;1S'l' <br /> <br />" <br />"", <br /> <br />" <br /> <br />6tZO <br /> <br />, <br /> <br />SW <br /> <br /> <br /> <br />7000 <br /> <br /> <br /> <br />Pe <br />~ <br /> <br />4000 <br /> <br />Pb <br /> <br />3000 <br /> <br />~ LEADVIlLE, UMESTONE <br />= DYER DOLOMITE AND <br />~ PARllNG fORMAllON <br />= DOTSERO FORMATION <br />= MANITOU DOLOMITE <br />~ SAWATCH QUARTZITE <br /> <br />~ PRECAMBRIAN GRANITE <br /> <br />> GROUNDWATER FLOW DIRECTlON <br /> <br />NO HORIZONTAL SCALE- <br />NOT BASED ON ACTUAL <br />STRUCTURES-DIAGRAMMATIC <br />PURPOSE ONLY. <br /> <br />DIAGRAMMATIC CROSS-8ECTION <br />AT GLENWOOD SPRINGS <br />Figure 4 <br />