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Last modified
11/23/2009 12:39:54 PM
Creation date
5/18/2007 4:39:56 PM
Metadata
Fields
Template:
Floodplain Documents
County
Boulder
Community
Boulder County and Incorporated Areas
Title
FIS - Boulder County and Incorporated Areas - Vol 1
Date
10/4/2002
Prepared For
Boulder County
Prepared By
FEMA
Floodplain - Doc Type
Current FEMA Regulatory Floodplain Information
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<br />On May 8 and 9, 1957, approximately 3 to 5 inches of rain <br />the entire basin of St. Vrain Creek. The rain <br />approximately 10 p.m. and stopped at approximately 6 a.m. <br />at approximately 1 a.m., St. Vrain Creek peaked at <br />3,060 cfs. The flood damaged and destroyed irrigation <br />works and bridges downstream fram Lyons. <br /> <br />fell over <br />began at <br />On May 9, <br />Lyons at <br />diversion <br /> <br />~n 1969, heavy rainfall combined with snowmelt caused prolonged high <br />flows OD St. Vrain Creek. The worst flooding occurred on May 7 <br />and 8 and from JuDe 15 to JuDe 21. Roads and bridges along the <br />stream were extensively damaged, streambanks were eroded, and <br />faruaands were flooded. On May 7, the peak discharge at Lyons was <br />2,900 cfs. (photographs of the 1969 flood are shown on Figures 17, <br />18, 19, and 20.) <br /> <br />The steep stream slopes create swift currents during a flood, which <br />produces added damages. Debris carried ~ the fast-moving water not <br />only threatens bridges and culverts, but batters houses or other <br />structures on the floodplain. The bridge and culvert crossings <br />often result in channel restriction, raising the water-surface <br />profile. Erosion undercuts and destroys structures which would <br />otherwise receive little damage fram inundation. Large quantities <br />of rocks are often deposited in portions of the channel, leaving <br />little capacity for future floods. Vegetative growth in the channel <br />also reduces the channel capacity and causes increased overbank flow <br />during high floods. Major flood damages in the study area are to <br />roads, culverts, and residential buildings. <br /> <br />Early records of floods in the Town of Nederland study area are <br />fragmented and lacking in detail. A description of the more-recent <br />floods follows: <br /> <br />June 22, 1951 - Boulder Daily Camera: <br /> <br />Nederland reservoir at the head of Boulder Canyon is full <br />for the first time in two years. <br /> <br />with water pouring over the 132-foot-high spillway at the <br />dam and heavy rains falling in the mountains, a flood <br />threat developed in Boulder Creek Thursday night but there <br />was little damage. Contrary to broadcast reports, the <br />water did not reach the canyon highway or cause any <br />interference with road bridges . . . It is not unusual for <br />the reservoir to fill; it has happened more than half of <br />the years since the dam was completed in 1910. But with <br />the dam unable to hold any more water, it means a possible <br />flooding of Boulder Creek if there are heavy rains and fast <br />thaws of snow at the headwaters. <br /> <br />27 <br />
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