Ð The procedure developed by SELLEVOLL (1989, 1992) and GRAHAM (1998, 1999) is used to estimate seismic hazard parameters in north Algeria. The area-speci®c seismic hazard parameters that were calculated consist of the b value of the Gutenberg±Richter frequency± magnitude relation, the activity rate k(M) for events above the magnitude M, and the maximum regional magnitude M max . These parameters were calculated for each of the six seismogenic zones of north Algeria. The site-speci®c seismic hazard was calculated in terms of the maximum possible PGA at hypothetical engineering structures (HES), situated in each of the six seismogenic zones with coordinates corresponding with those of the six most industrial and populated cities in Algeria.