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Last modified
11/23/2009 1:42:34 PM
Creation date
10/4/2006 9:35:50 PM
Metadata
Fields
Template:
Floodplain Documents
County
Mesa
Community
Collbran
Stream Name
Plateau Creek
Title
Plateau Creek Flood Analysis
Date
1/1/1984
Prepared For
Mesa County
Prepared By
Greenhorne & O'Mara, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />II <br />II <br />II <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />to the U.S. Army Corps of Engineers' design guidelines for levees which would <br />make it impermeable and would add two more feet of freeboard. <br /> <br />Area 3 - Three structures here could be affected if flows equal to or <br />greater than the 100-year event occurred. With the levee on the south stream <br />bank, water would flow over the road on the north side, but at depths of less <br />than one foot. If high waters threaten the structures they can be protected by <br />a temporary local measure like sandbagging. <br /> <br />Area 4 - Just below the confluence of Buzzard Creek with Plateau Creek the <br />channel is quite shallow and therefore has a limited capacity. Without the <br />existing levee and sandbags already in place the channel could handle only 1900 <br />cfs or the 4-year flood event. By making the existing levee permanent the two <br />structures in these areas could be protected from flows in excess of the 100- <br />year event. As in Area 2, the levee should be constructed according to Corps of <br />Engineers' design guidelines. <br /> <br />Area 5 - This property was threatened through bank erosion during last <br />years runoff. With the change in stream channel location in this area, the <br />erosion threat is somewhat reduced, however, consideration should be given to <br />riprap bank protection along the southeast corner of the property as a permanent <br />protection measure. <br /> <br />STREAM MONITORING <br /> <br />Some form of stream flow monitoring is recommended for Plateau and Buzzard <br />Creeks, especially during snowmelt season, in order to keep track of the rising <br />and falling trends of the flood peaks. In addition to serving as an indicator <br />of an ensuing flood event, the stream gage records, over a number of years, will <br />serve as a point of reference. After a few years a range of "normal" runoff <br />values will become evident and excessively high flows can be identified as an <br />indicator of a potential flooding situation. <br /> <br />The flow monitoring device recommended i5 a staff gage. This could be a <br />board mounted on one of the bridge abutments marked off in even increments or <br />the markings could be painted directly on the abutment. The marks should be at <br />one foot intervals with 0.1 or 0.2 foot subdivisions. To properly relate to the <br />rating curves (Figures 1 and 2) developed at the bridges, the zero mark on each <br />staff gage should be the same elevation as the channel invert. These gages will <br />not be very sensitive to low flows but they should be adequate for their <br />intended purpose; estimating flows and tracking the rate at which the water <br />level rises du~ing high flow periods. <br /> <br />4 <br />
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