Southeast Florida does not shake like California, but the seismic hazard in Fort Lauderdale is governed by long-period motion from distant sources and by the local soil column. The IBC classifies much of Broward County as Site Class D or E, and the ASCE 7-22 ground motion maps assign a uniform-hazard spectrum that requires site amplification factors Fa and Fv. A seismic microzonation study in Fort Lauderdale goes beyond the code default by mapping shear-wave velocity profiles with MASW and correlating them with SPT N-values from sondajes SPT, delivering a block-by-block prediction of ground shaking that feeds directly into foundation design and retrofit prioritization.
A site-specific spectrum in Fort Lauderdale can reduce design base shear by 15% or reveal a hidden Class E penalty of 20%—both numbers that change the structural system.
