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Board Meeting 10/01/1987
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Board Meeting 10/01/1987
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8/16/2009 3:15:53 PM
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10/4/2006 7:15:29 AM
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Board Meetings
Board Meeting Date
10/1/1987
Description
CWCB Meeting
Board Meetings - Doc Type
Meeting
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<br />. <br /> <br />Rule 6. <br /> <br />. <br /> <br />. <br /> <br />Standards for <br />Information: <br />information. <br />consideration <br />subject to <br />respectively. <br /> <br />Delineation of Approximate Floodplain <br />To qualify as approximate floodplain <br />the standards of this rule with <br />of the effects of dams and levees being <br />the criteria of rules 7 and 8. <br />must be met. <br /> <br />A. Topographic Base Mapping. <br /> <br />1. Work Map. The best available topographic <br />base map shall be used to develop approximate <br />floodplain information. Such work map shall. <br />at a minimum. be the most recent edition of a <br />7.5 minute quadrangle as published by the U.S. <br />Geological Survey (USGS). <br /> <br />B. Hydrologic Analysis <br /> <br />1. Frequency. The hydrologic analysis for the <br />preparation of approximate floodplain <br />information shall include. at a mlnlmum. <br />calculation of the lOO-year frequency flood <br />peak discharge. <br /> <br />2. Other Requirements. The hydrology for <br />approximate floodplain information shall. at a <br />minimum. meet the hydrology standards in rule <br />5.B.2 through 5.B.6. for detailed floOdplain <br />information. <br /> <br />C. Hydraulic Analysis <br /> <br />1. <br /> <br />Floodplain <br />area maps <br />floodplain <br /> <br />Boundaries. Approximate flooded <br />shall show. at a mlnlmum. the <br />boundary for the lOO-year flood. <br /> <br />2. MethodoloQY. Approximate flooded area maps <br />shall be based on the following simplified <br />methods. or any other method approved by the <br />Board. either individually or in combination. <br />as appropriate: <br /> <br />a. Assumed Depth Method. An assumed flood <br />depth above the channel may be used in <br />conjunction with the best available <br />topographic map. The assumed depth may be <br />determined from a regional regression <br />analysis of depth-frequency relations or <br />from the slope-area-conveyance calculation <br />at representative cross sections. Where <br /> <br />-19- <br />
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