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2. STUDY AREA CHARACTERISTICS <br /> <br />TABLE 2.2.3-1 <br />Historical Seismic Events That Have Occurred Within 60t Miles of the MWMC Service Area2 <br />MWMC Facilities Plan, Eugene-Springfield <br /> <br /> Latitude Longitude Distance <br /> Year Month Day (o North) (o West) Magnitude3 Intensity4 (miles) <br /> <br /> 2004 2 26 45.65 122.75 3.0 IIIF 43.5 <br /> <br />1The approximate center of the MWMC service area is located at latitude 45° 05' 00' N, longitude 123° 07' 00" <br />W. <br />2 Soume: USGS Earthquake Hazards Program (see http://neic.usqs.qov/neis/epic/epic_circ.html). The database <br />search included Significant U.S. Earthquakes 1568 to 1989 and USGS/NEIC (PDE) 1973-Present. The only <br />earthquakes in the database recorded prior to 1953 include two events, in 1892 and 1896. <br /> <br />3 Magnitude values are calculated by the USGS. Magnitude values are Local Magnitudes (LM) and Coda <br />Duration Magnitude (MD). ML magnitude is generally referred to as the true "Richter magnitude." The values are <br />computed for distances less than 600 km with depths less than 70 km. MD estimates are derived from the <br />duration or coda length of earthquake vibrations. Duration or coda magnitude scales are normally adjusted to <br />agree with ML(see http://neic.usgs.gov/neis/epic/code_magnitude.html). <br /> <br />4 Modified Mercalli intensity scale. Dashed line equals no data for that event. <br /> <br />Based on information from the USGS database, numerous small earthquakes with <br />magnitudes between 3 and 5 have occurred with 60 miles of the MWMC service area during <br />historical times. The closest earthquakes were magnitude 5.0 and 3.4 events that occurred <br />12.4 and 13.7 miles from the approximate center of the service area. The largest historical <br />event was an estimated magnitude 5.7 earthquake that occurred in 1993, approximately <br />21 miles from the center of the service area. As noted above, the two largest earthquakes in <br />recent years in Oregon include the Scotts Mills, (magnitude 5.6) and Klamath Falls quakes <br />(magnitude 5.9 and magnitude 6.0) of 1993 (both earthquakes were beyond the 60-mile <br />radius noted in Table 2.2.3-1) <br /> <br />According to the Uniform Building Code Seismic Risk Map of the United States, the <br />Eugene-Springfield metropolitan area (and most counties west of the crest of the Cascades, <br />including the Willamette Valley and the Portland Metro area) are located in Seismic Zone 3 <br />(bBC, 1997). This seismic zone corresponds to an intensity VIII earthquake on the MM Scale. <br />An intensity VIII earthquake can produce slight damage in specially designed structures to <br />considerable damage in ordinary substantial buildings, with partial collapse(see Table <br />2.2.3.2). <br /> <br />An earthquake magnitude of 9.0 was selected as being the controlling event at the Project <br />site (USGS, 2003). The earthquake magnitude selected for the Project site was based on <br />USGS deaggregation seismic hazard mapping for the Eugene-Springfield metropolitan area. <br />The latitude and longitude of the approximate center of the site was entered into the USGS <br />database to obtain seismic magnitude probability for the Project location. The USGS seismic <br />hazard maps present the average magnitude of all potential sources at a given location, and <br />provide the percent contribution at discrete locations of the overall seismic hazard. This <br />magnitude event (9.0) corresponds to a 475-year mean return interval. <br /> <br />Seismic ground acceleration for the Project site was determined according to the National <br />Earthquake Hazards Reduction Program (NEHRP) maps for probabilistic ground motion <br /> <br />MWMC_2.0_REV23.DOC 2-9 <br /> <br /> <br />