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Errata |
U.S. Geological Survey
MS 966, Box 25046
DFC
Denver,
Colorado, 80225
Bulletin of the Seismological Society of America, Vol. 89, No. 2, pp. 468483, April 1999
In Frankel et al. (1999), we incorrectly described part of the shear-wave velocity (Vs) profile used to calculate the predicted spectra at site KD1 near the Kingdome in Seattle (figure 7 of Frankel et al., 1999). The shear-wave velocity profile we used was partially determined from a seismic refraction/reflection survey reported by Williams et al. (1999) at sites KD1 and KD2. The velocity of the stiff deposits underlying the fill was taken from a borehole measurement at a nearby location (Shannon and Wilson, unpublished report, 1994). The shear-wave velocity profile consisted of a 19-m-thick layer of fill and recent alluvium with Vs of 145 m/sec over a 1.1-km-thick layer of stiff Pleistocene deposits, with Vs of 579 m/sec over a half-space, with Vs of 1.0 km/sec (bedrock). The thickness of the top layer was determined by Williams et al. (1999) from the timing of a strong shear-wave reflection observed in their survey and the velocity of the initial S-wave arrival. This reflection is from the interface between the overlying artificial fill and the stiff soil unit beneath. As reported in Williams et al. (1999), the two-way travel time observed from the reflection survey (0.265 sec) is consistent with the 2 Hz resonance observed in the earthquake data by Frankel et al. (1999). The error in our description of the profile does not affect the results reported in our article.
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Frankel, A., D. Carver, E. Cranswick, M. Meremonte, T. Bice, and D.
Overturf (1999). Site response for Seattle and source parameters
of earthquakes in the Puget Sound region, Bull. Seism. Soc.
Am. 89,468
483.
Shannon and Wilson (1994). Kingdome seismic evaluation, Seattle, Washington. Report W-6836-01, Seattle, Washington, unpublished report.
Williams, R. A., W. J. Stephenson, A. D. Frankel, and J. K. Odum (1999). Surface seismic measurements of near-surface P- and S-wave seismic velocities at earthquake recording stations, Seattle, Washington, Earthquake Spectra 15,565 584.[CrossRef]
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