This probabilistic seismic hazard analysis for The Netherlands is base
d on the catalogue of European earthquakes published by the Commission
of the European Communities. The seismic hazard is assessed by applyi
ng a modified version of the McGuire program. This method uses for eac
h seismotectonic zone a linear frequency-intensity relation, an upper
bound of intensity, an average depth for large earthquakes and an azim
uth-dependent attenuation. It assumes a Poisson process for large eart
hquakes. The annual probability versus intensity is calculated for sit
es at gridpoints with 7 km spacing. Hazard intensity maps are presente
d for the annual probabilities of occurrence 0.02, 0.01, 0.005, 0.001,
0.0004 and 0.0001. A rough estimate of the error is approximately one
half of an intensity unit for all probabilities. The highest seismic
hazard in The Netherlands is found in the south-east with intensity VI
II for a 0.0001 annual probability and is decreasing to the north-west
in line with the seismicity.