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<br />o <br />I\,) <br />o <br />-.J <br /> <br />7000 <br /> <br />Lookout <br />Mountain <br /> <br />7000 <br /> <br />600 <br /> <br /> <br />Glenwood Springs <br /> <br />6000 <br /> <br />Belden & Molas Fms. <br /> <br />6000 <br /> <br />5000 <br /> <br />Granite <br /> <br />4000 <br /> <br />4000 <br /> <br />o \ <br /> <br />I 5000 Feet <br /> <br />Figure 1. Geological cross section running through Glenwood Springs following <br />the general direction of the Colorado River (NW-SE). The structure beneath <br />Glenwood Springs is anticlinal with keystone faulting at the crest. Note that the <br />Leadville Limestone is a regional aquifer. (from Geldon, 1989, modified) <br /> <br />4 <br />