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<br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Summer of 1981 <br /> <br />The city had a reprieve from heavy storm damages until the summer of 1981, <br />when a series of afternoon thunderstorms moved into the valley and began its <br />cycle of mud and debris flows again. <br />Some things had changed during the four years between cloudburst generated <br />storms. Some of city personnel were newly hired so some clean-up was done <br />differently. The all-volunteer fire department had a paid chief, and mitigating <br />work, such as berms, had been done by some homeowners, diverting flows from <br />their property. However, this just changed the flow to someone else. Some <br />records were kept in different ways, but costs were still high. <br />Since the Glenwood Springs area has rock units of the Maroon Formation and <br />the Eagle Valley Evaporite, this settling causes frequent, large mud and debris <br />flows. <br />Soils formed from the Eagle Valley Evaporite absorb water easily and change <br />to thick slurries which are relatively mobile and flow to considerable distances <br />on debri s fans. <br />Maroon rocks decompose with weathering, forming accumulations of boulders, <br />smaller rock fragments, and silt, clayey silt and sand. Upon saturation and <br />