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<br /> <br />2021 Multijurisdictional Local Hazard Mitigation Plan <br /> <br />10.2.3 Frequency <br />Historical records of earthquake occurrences give some indication of future probabilities. Seismic activity was <br />more frequent from 1830 to 1930 than it has been since. This leads some scientists to suspect that pressure is <br />building up along the faults in the Bay Area that can result in a large quake. Such a quake could have dramatic <br />and devastating effects throughout the Bay Area. The USGS reports the following earthquake probabilities for the <br />Bay Area over next 30 years (U.S. Geological Survey, n.d.): <br /> 72 percent probability of an earthquake measuring magnitude 6.7 <br /> 51 percent probability of an earthquake measuring magnitude 7 <br /> 20 percent probability of an earthquake measuring magnitude 7.5 <br />The Third Uniform California Earthquake Rupture Forecast identified recurrence intervals for four deterministic <br />scenarios applicable to San Mateo County (Working Group on California Earthquake Probabilities, 2021): <br /> San Andreas Fault scenario, recurrence interval = 160 years <br /> San Gregorio Fault Scenario = 481 years <br /> Butano Fault Scenario = 2,881 years <br /> Monte Vista Fault Scenario = 1,894 years <br /> <br />10.2.4 Severity <br />The severity of an earthquake can be expressed in terms of intensity or magnitude (see Section 10.1.3). The State <br />of California Department of Conservation probabilistic ground shaking maps, based on current information about <br />fault zones, show the PGA that has a certain probability of being exceeded in a 50-year period. San Mateo County <br />is in a high-risk area, with a 10-percent probability in a 50-year period of ground shaking from a seismic event <br />exceeding 60 percent of gravity in some parts of the County. Figure 10-5 shows the expected peak horizontal <br />ground accelerations for this probability. <br /> <br />10.2.5 Warning Time <br />There is no current reliable way to predict the day or month that an earthquake will occur at any given location. <br />Research is being done with warning systems that detect the lower energy compressional waves (P waves) that <br />precede the secondary waves (S waves) experienced as an earthquake. Earthquake early warning systems may <br />provide a few seconds’ or a few minutes’ notice that a major earthquake is about to occur. The warning time is <br />very short, but it could allow for someone to get under a desk, pause hazardous or high-risk work, or initiate <br />protective automated systems in critical facilities. <br /> <br />10.3 EXPOSURE <br />10.3.1 Population <br />The entire population of the planning area is potentially exposed to direct damage from earthquakes or indirect <br />impacts such as business interruption, road closures, and loss of function of utilities. <br /> <br /> <br /> <br /> <br /> <br />10-12