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Veotechnical Engineering Study <br />Oa-2267 Three Story Addition - 500 Laurel Street, Everett <br />January 31, 2001 <br />Seismic Risk <br />While we did not perform a datailed seismic risk analysis for this project, it is clear <br />that earthquake ground motion response is a partic�lariy important factor and that <br />it should be carefully considered in structural design. Historically, th� Puget Sound <br />Region has been :�ubjected to frequent earthquakes of modeiate intensity, and is <br />designated in the Uri`omi Building Code as Seismic Zone 3. Two earthquakes that <br />resulted in significani damage occurred in 1949 near Olympia, and in 1965 near <br />Seattle. The April 3, 1949 earthquake is the largest recorded earthquake in the <br />region, reachiny a magnitude of 7.1. It was felt over 150,000 square miles, <br />resultiny in $25 million in damages, eight (8) deaths and many injuries. The Ap�il <br />29, 1965 earthquake of magnitude 6.5 was felt over 130,G00 square miles, and <br />resulted in widespread damage in the Seattle area. The area was also subjected <br />to a Magnitude 5.0 earthquake during January 1995 and a 5.4 earthquake in May <br />of 1996, and more recently a 5.9 earthquake. <br />Based on seismic risk analyses we have performed for similar sites in the Puget <br />Sound region, considering the generally fi��m nature of the majority of the in-situ <br />materials, and using the criteria contained in the City of Seattle Directors Rule 3-93 <br />(the current state of the practice in this area for unsophisticated seismic analyses), <br />we estimate that the design peak horizontal ground acceleration at the site should <br />be considered to be o� the arder of the followiny: <br />■ Minirnum lateral acceleration = 0.17g <br />Approximate acceleration levels are only estimatable at this time for the state of <br />practice due to complexities of the area ±hat could iiiclude focusirg and other <br />complex concepfs. <br />Figure 16.2 of the 1997 eoiition of the Unifo.m Building Code (UBC) also indicates <br />that the site is located within the seismic area desionated as Seismic Zone 3. For <br />this zone the UBC indicates in Table 16-I that the site has the following zone factor: <br />1997 UBC Seismic Zone factor, 7 = 0.30 <br />37 <br />J <br />I <br />I <br />� <br />1 <br />1 <br />I <br />� <br />1 <br />1 <br />1 <br />