A global seismic hazard assessment was conducted using the probabilist
ic approach in conjunction with a modified means of evaluating the sei
smicity parameters. The earthquake occurrence rate function was formul
ated for area source cells from recent instrumental earthquake catalog
s. For the statistical application of the G-R relation of each source
cell, the upper- and lower-bound magnitudes were determined from, resp
ectively, historical earthquake data using a Kernel smoothing operator
and detection thresholds of recent catalogs. The seismic hazard at a
particular site was obtained by integrating the hazard contribution fr
om influencing cells, and the results were combined with the Poisson d
istribution to obtain the seismic hazard in terms of the intensity at
10% probability of exceedance for the next 50 years. The seismic hazar
d maps for three countries, constructed using the same method, agree w
ell with the existing maps obtained by different methods. The method i
s applicable to both oceanic and continental regions, and for any spec
ific duration of time. It can be used for those regions without detail
ed geological information or where the relation between existing fault
s and earthquake occurrence is not clear.