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FLOOD09982
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Last modified
1/26/2010 10:11:22 AM
Creation date
10/5/2006 4:47:20 AM
Metadata
Fields
Template:
Floodplain Documents
County
Garfield
Community
Battlement Mesa
Stream Name
Colorado River
Basin
Colorado Mainstem
Title
Battlement Mesa Storm Drainage and Floodplain Study
Date
3/1/1975
Prepared For
CWCB
Prepared By
Frasier & Gingery, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />II <br />I <br />, <br /> <br />I II <br />: II <br />II <br />II <br /> <br />Page Thirteen <br />Battlement Hesa Development Storm Drainage and Flood Plain Study <br /> <br />In liaht of thE' Corps studies and knowledge of the area, <br />the 6.5 cfs per square mile of tributary area was used to esti- <br />mate the lOa-year flood maanitude at Grand Valley. This approach <br />is consistent ~ith procedures outlined by the Federal Insurance <br />Administration. This approach results in a laO-year flood magni- <br />tude of approximately 47,500 cfs at this point on the Colorado <br />River. This fiaure has been adopted for preliminary design and <br />floodplain evaluation. <br /> <br />IX. Flood Plain lnalysis Procedure <br /> <br />The actual floodplain as shown on Drawings 926.010, <br />Flood Plain Plan and Profile, has been calculated using the <br />Corps of Engineers COJ11puter Program EEC-2, Hater Surface <br />Profiles. The proaram represents the most advanced, flexible, <br />and accurate J11ethod of establishing floodplain profiles. <br />The proaraJ11 is used by the Corps of Engineers for their <br />Flood Information Peports and by the Federal Insurance Pdminis- <br />tration for preparation of detailed flood hazard zones for <br />the flood insurance program. <br /> <br />River cress sections were obtained by field survey <br />methods in Octcber, 1974. The cross sections were taken from <br />the water surface to a point approxiJ11ately 20 feet above the <br />wa ter levE'l. <br /> <br />No soundings of the river bottom were taken. Instead, <br />a theoretical bottom section 'vas developed which would <br />reasonably convey the 2,000 cfs base flow at the time of the <br />survey. The base flow represents approximately 4% of the 100- <br />year discharae. Therefore, the actual river cross section <br />below the water level has relatively little effect on the 100- <br />year flow. Based on average slopes and cross sections throuqh <br />the study area, it was determined that 500 to 700 square feet <br />should be added to each cross section below the water surface <br />to compensate for the flow at the time of survey. <br /> <br />Hydraulic COefficients selectecJ for the backwater <br />calculations are as follows: <br /> <br />r'lanninqs "n" value - Channel <br />Manninas "n" value - Overbank Area <br />Grassed <br />Mannings "p" value - Overbank Area <br />Prea with Dense Brush <br />Expansion Loss Coefficient <br />Contraction Loss Coefficient <br /> <br />0.040 <br /> <br />0.045 <br /> <br />0.100 <br />0.500 <br />0.300 <br /> <br />I' <br /> <br />. <br />
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