Item talk:Q72256
From geokb
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"name": "Intensity distribution and isoseismal maps for the Nisqually, Washington, earthquake of 28 February 2001",
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"abstract": "We present isoseismal maps, macroseismic intensities, and\r\ncommunity summaries of damage for the MW=6.8\r\nNisqually, Washington, earthquake of 28 February, 2001.\r\nFor many communities, two types of macroseismic intensity\r\nare assigned, the traditional U.S. Geological Survey\r\nModified Mercalli Intensities (USGS MMI) and a type of\r\nintensity newly introduced with this paper, the USGS\r\nReviewed Community Internet Intensity (RCII). For most\r\ncommunities, the RCII is a reviewed version of the\r\nCommunity Internet Intensity (CII) of Wald and others\r\n(1999). For some communities, RCII is assigned from\r\nsuch non-CII sources as press reports, engineering reports,\r\nand field reconnaissance observations. We summarize differences\r\nbetween procedures used to assign RCII and\r\nUSGS MMI, and we show that the two types of intensity\r\nare nonetheless very similar for the Nisqually earthquake.\r\nWe do not see evidence for systematic differences between\r\nRCII and USGS MMI that would approach one intensity\r\nunit, at any level of shaking, but we document a tendency\r\nfor the RCII to be slightly lower than MMI in regions of\r\nlow intensity and slightly higher than MMI in regions of\r\nhigh intensity. The highest RCII calculated for the\r\nNisqually earthquake is 7.6, calculated for zip code 98134,\r\nwhich includes the ?south of downtown? (Sodo) area of\r\nSeattle and Harbor Island. By comparison, we assigned a\r\ntraditional USGS MMI 8 to the Sodo area of Seattle. In\r\nall, RCII of 6.5 and higher were assigned to 58 zip-code\r\nregions. At the lowest intensities, the Nisqually earthquake\r\nwas felt over an area of approximately 350,000 square km\r\n(approximately 135,000 square miles) in Washington,\r\nOregon, Idaho, Montana, and southern British Columbia,\r\nCanada. On the basis of macroseismic effects, we infer\r\nthat shaking in the southern Puget Sound region was\r\nsomewhat less for the 2001 Nisqually earthquake than for\r\nthe Puget Sound earthquake of April 13, 1949, which had\r\nnearly the same hypocenter and magnitude. Allowing for\r\ndifferences in hypocenter, shaking in the 2001 earthquake\r\nwas very similar to that produced by the Puget Sound\r\nearthquake of April 25, 1965. First-person accounts of the\r\neffects of the 2001 earthquake on individual households\r\nare given for some communities.",
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