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<br />HISTORY OF THE DAMS <br /> <br />9 <br /> <br /> <br />FIGURE G.-The remains of the outlet valve from Lawn Lake dam. Investigations of this valve led to the conclusion <br />that lead caulking had severely deteriorated. <br /> <br />material. Campers in the vicinity of Lawn Lake the <br />night before the failure reported hearing a noise that <br />sounded like strong winds. This sound indicated that <br />the reservoir may have been discharging through the <br />dam for at least 3 to 4 hours before the hole enlarged <br />sufficiently-or embankment failure occurred-above <br />the outlet pipe, causing a total breach of the dam where <br />the outlet works were located (figs. 7A,B). <br />Surveyed breach dimensions are: Depth of 28 ft, top <br />width of 97 ft, and bottom width of 55 ft. Following the <br />complete failure of the dam embankment at about 0530 <br />MDT, the resulting outflow of water reached its peak dis- <br />charge very quickly (estimated to be within 10 minI. The <br />resulting flood peak of 18,000 ftSts (see "Dam-Break <br />Modeling") then proceeded down the Roaring River <br />toward Horseshoe Park and the Cascade Lake dam. <br /> <br />CASCADE LAKE DAM <br /> <br />Cascade Lake dam, a concrete gravity dam, was <br />located on the Fall River in Rocky Mountain National <br />Park, 5.3 mi west of Estes Park (fig. 1). A diversion <br /> <br />dam was originally constructed at the site in 1908 for <br />a pipeline to a hydropower plant downstream. The <br />powerplant supplied electricity to the Stanley Hotel <br />and the town of Estes Park. The site was at the head <br />of a steep drop with numerous rapids and large boul- <br />ders in the Fall River, where the stream eroded through <br />several Pleistocene terminal moraines that dammed <br />the Fall River, creating a glacial lake in Horseshoe Park <br />just upstream. Cascade Lake dam consisted of a con- <br />crete wall several feet thick, reinforced with a masonry <br />rock buttress on the downstream side. The founda- <br />tion and abutments were in glacial terminal-moraine <br />sediments; no bedrock is evident in the foundation. A <br />photograph at Cascade Lake dam is shown in figure 8. <br />The dam was acquired in 1945 by the town of Estes <br />Park, which owned it at the time of failure. Various im- <br />provements were made on the structure. It was enlarged <br />to 17 ft high in 1923. The reservoir behind the dam was <br />dredged at least twice since 1945, most recently in <br />November 1981. Postfailure surveys indicated that the <br />water behind Cascade Lake dam was approximately <br />12 ft deep, and the dam was 143 ft long prior to failure. <br />Because of the sediment accumulation of 5 ft, a height <br />