“…For example, it may not be possible to accurately define the statistical distribution on the attenuation laws in the eastern United States where strong motion data records are at a premium. This will make it necessary to extrapolate western data for use in the east, assuming that corrections can be made for the different attenuation properties of the two regions[3].Many assumptions will also have to be made in defining other geo-seismic models. Specification of source zones, upper and lower bound magnitudes, the location of the source relative to the site, and so on, are all fraught with uncertainty and bias.…”