“…Six ground motion ensembles were utilized; each ensemble has 20 ground motions that aggregate earthquake events of different magnitudes and epicentral distances and collectively represent ground motions with probabilities of 10%/50-yr (la01-20, se01-20, bo01-20 for Los Angeles, CA, Seattle, WA, and Boston, MA, respectively) and 2%/50-yr (la21-40, se21-40, and bo21-40). For residences in St Louis, MO, which is located within 150 miles of multiple earthquake sources including the New Madrid Seismic Zone (NMSZ), synthetic ground motion ensembles generated by Wen and Wu [18] having exceedance probabilities of 10% and 2% in 50-yr were used. The dispersion in the response spectra from ground motions la21 through la40 for Los Angeles, illustrated in Figure 4, represents the uncertainty in the random amplitude and phasing from an ensemble of ground motions corresponding to a return period of approximately 2500 years.…”