Experiments on the attenuation of Rayleigh waves in a marble quarry by a pe
riodic array of cylindrical holes, in a honeycomb and in a triangular distr
ibution, are reported. The results are explained in terms of elastic wave c
rystals (EWC's), and compared to theoretical calculations performed with sc
alar waves. The scaling property of the underlying theory has led us to exp
lore the possible application of the results obtained to the attenuation of
surface waves in seismic movements.