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<br />7000 <br /> <br />6000 <br /> <br />t; <br />w <br />... <br />~ 5000 <br />~ <br />ti <br />1/1 <br /> <br />4000 <br /> <br />3000 <br /> <br />" <br />" <br /> <br />l.vZO <br /> <br />NW <br /> <br />LOOKOUT <br />MTN. <br /> <br /> <br />REDSTONE <br />WELL <br /> <br />Pe <br /> <br />P€g <br /> <br />(AFTER GELDEN, 1989) <br /> <br />IQ;;l STREAM TERRACE AND <br />'-=-l CHANNEL AU.lMUM <br /> <br />~ lEADVlu.E UIIESTONE <br />= DYER DOLOMITE AND <br />~ PARTING FORlAAnON <br />= DOlSERO FORlAAnON <br />= MANITOU DOLOMITE <br />~ SAWATCH QUARIZITE <br /> <br />lpegl PRECAMBRIAN GRANITE <br /> <br />> GROUNDWATER FLOW DIRECTION <br /> <br />SCALE IN FEET <br />VERTICAL EXAGGERATION X2 <br /> <br />~ <br />~ <br />[B <br />@] <br /> <br />SLOPE AU.lMUM <br />MAROON FORMAnON <br /> <br />o <br /> <br />2000 4000 <br /> <br />EAGLE VAlLEY EVAPORITE <br />BElDEN AND MOlAS <br />FORMAnON <br /> <br />Michael J. Galloway <br />COII8Vl.17JH1 ITnlffJQOUJCl8'f <br /> <br />SW <br /> <br />7000 <br /> <br />6000 <br /> <br />t; <br />w <br />... <br /> <br />5000 ~ <br />~ <br />ti <br />III <br /> <br />4000 <br /> <br />3000 <br /> <br />GEOLOGY AND STRUCTURE <br />AT GLENWOOD SPRINGS <br />Figure 2 <br />