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<br /> <br />2021 Multijurisdictional Local Hazard Mitigation Plan <br /> <br />Principal flooding sources for San Mateo County as identified on FEMA flood maps include the following <br />streams and water bodies: <br /> Alpine Creek <br /> Belmont Creek <br /> Butano Creek <br /> Colma Creek <br /> Crystal Springs <br />Channel <br /> Denniston Creek <br /> El Granada Creek <br /> Holly Street Channel <br /> La Honda Creek <br /> Lomita Channel <br /> Montara Creek <br /> Pacific Ocean <br /> Pescadero Creek <br /> San Bruno <br />Channel <br /> San Francisquito <br />Creek <br /> San Gregorio Creek <br /> San Vincente Creek <br /> Woodhams Creek <br /> <br />Over 20 creeks, channels, and water bodies, including those identified as principal flooding sources, were <br />assessed as part of the County’s FIS. In addition to the waterways above, the FIS identified areas at risk for <br />potential tsunami inundation. The Cities of Half Moon Bay and Pacifica are both associated with potential <br />tsunami issues. Additional information regarding the tsunami hazard is in Chapter 15. <br /> <br />Investigation of San Mateo County’s vulnerability to flooding can also include assessments of watershed <br />locations. Every watershed has unique qualities that affect its response to rainfall. San Mateo County contains 34 <br />watersheds, all of which are relatively small and drain into either the Pacific Ocean or San Francisco Bay. <br />Unincorporated areas in the County contain 21 major watersheds. Except for Crystal Springs and San <br />Francisquito, which both drain into the San Francisco Bay, all the rural watersheds drain into the Pacific Ocean <br />(San Mateo County OES, 2015). <br /> <br />11.2.3 Principal Flood Problems <br />The 2019 Flood Insurance Study (FIS) for San Mateo includes a description of the principal flood problems that <br />have been noted for San Mateo County, by flooding source, as summarized in Table 11-3. <br /> <br />Table 11-3. Summary of Flood Problems <br />Source Description of the Flood Problem <br />All Sources Flooding is predominantly shallow along streams on the bayside of San Mateo County. Spills from channels flow <br />independently through the urbanized areas, usually following streets, and result in flood depths of less than 1 foot. <br />Occasionally, railroad or highway embankments form barriers, resulting in deeper ponding or sheet flow flooding. <br />Flooding on the ocean side of the county is predominantly confined to well-defined riverine valleys, with flood surface <br />extending uniformly across the floodplain <br />Colma Creek The Daly City storm drain terminates in a junction structure near the intersection of F Street and El Camino Real. <br />Because the downstream storm drain has only one-half the waterway area of the upstream storm drain, the excess <br />flow is forced from the storm drain through a side channel into the Colma Mobile Home Park on the northwestern side <br />of the intersection, where it ponds. <br />San Bruno, <br />Crystal Springs, <br />and Lomita <br />Channels <br />Shallow flooding zones between the Bayshore Freeway and the mainline of the railroad are the result of overland <br />flows from San Bruno Channel and Crystal Springs Channel. These flows merge behind the railroad embankment and <br />eventually cross the railroad tracks as independent flows. Approximately 220 cubic feet per second (cfs) flows into the <br />area north and west of the Crystal Springs Channel and is pumped into the channel at a rate of 35 cfs. The Crystal <br />Springs Channel itself has a capacity of 200 cfs and is adequate for the flows reaching it. Approximately 740 cfs flows <br />into the area south of the Crystal Springs Channel and west of the Bayshore Freeway. This flow moves south until it <br />reaches Lomita Channel, where it is pumped into the Millbrae (High Line) Canal and flows to San Francisco Bay. The <br />Crystal Springs Channel (200-cfs flow) and the Belle Air storm drain (750-cfs flow) merge at San Bruno Avenue and <br />flow northeasterly to San Francisco Bay in the San Bruno Channel (1,000-cfs flow). The shallow flooding zone <br />adjacent to the San Bruno Channel is caused by local runoff. <br /> <br /> <br /> <br />11-8