The frequency-intensity and the frequency-magnitude relations are calc
ulated from the observed tectonic earthquakes in the Netherlands. The
obtained mean return periods for an intensity VII and a magnitude 5.8-
5.9, like the 1992 Roermond earthquake, are estimated to be 132 years
and 1000 years or more respectively. The influence of the recent Roerm
ond earthquake on the existing seismic hazard intensity maps for the N
etherlands is negligible. The earthquake hazard for the town of Roermo
nd is evaluated.