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Last modified
1/26/2010 2:27:11 PM
Creation date
10/12/2006 2:19:37 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
5930
Description
Flood Protection Section - Flood Events - By Year and Event
State
CO
Basin
Statewide
Date
8/6/1982
Author
Estes Park-Larimer C
Title
Lawn Lake Dam Failure and Fall River Flood - Estes Park and Larimer County Colorado
Water Supply Pro - Doc Type
Report/Study
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<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 />~J1127 <br /> <br />PART II <br />BACKGROUND INFORMATION <br /> <br />A. HISTORY OF LAWN LAKE DAM <br /> <br />The Lawn Lake Dam, located approximately 10 miles northwest of <br />Estes Park, was constructed in 1902. Original storage and re- <br />charge rights were granted on March 18, 1912, for the contain- <br />ment of 759.6 acre feet of water. Lawn Lake was a natural lake <br />but its elevation was raised by the construction of the earthen <br />dam. The storage rights and dam are owned by the Farmer's <br />Irrigation Ditch and Reservoir Company of Loveland, Colorado. <br />The area of Lawn Lake was included within Rocky Mountain National <br />Park when the Park was established by Congress on January 26, <br />1915. The storage reservoir was used to supply irrigation re- <br />serves to agricultural producers of the high plains of northeast <br />Colorado during the summer growing season. It is estimated that <br />Lawn Lake contained approximately 817 acre feet of water at the <br />time of the dam failure. <br /> <br />B. DRAINAGE BASIN HYDROLOGY AND FLOOD PROBLEMS <br /> <br />Estes Park is located at the confluence of the Big Thompson and <br />Fall Rivers. The town is surrounded by National Park and Nation- <br />al Forest lands. The climate can best be described as high- <br />altitude and semi-arid with all the attending ramifications of <br />such a classification: sudden and violent thunderstorms, flash <br />floods, heavy upstream snowpacks, and the critical need for stor- <br />age reservoirs. Even though violent storms are frequent, the <br />National Weather Service stresses that the July 15 flood event <br />was not caused by meteorological conditions. (ATTACHMENT 4) <br />The Fall River through and above Estes Park is typical of mountain <br />streams. It has heavy vegetation along the banks of the channel, <br />a cobbled stream bed, large rock outcroppings, steep channel <br />slopes and has the potential for high water velocities. The Fall <br />River drainage area at the confluence is 39.9 square miles. The <br />Big Thompson at this point drains 137 square miles. <br /> <br />The Fall River has a history of flooding. High streamflows have <br />been recorded in 1949, 1951, 1953, 1957, and 1965. Damages from <br />the 1965 event were the result of encroachment upon the river <br />channels and blockage of the river through the central business' <br />district. The Big Thompson disaster of August 1976 was the last <br />major flooding in the area, but it did not directly affect Estes <br />Park in terms of physical damages. A previous dam failure in <br />the area occurred on May 25, 1951 when Lily Lake dam collapsed <br />causing flooding along Fish Creek, a direct tributary to Lake <br />Estes. <br /> <br />4 <br />
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