The desire to operate denser networks in order to monitor seismic acti
vity at lower thresholds leads to greater emphasis on automated data p
rocessing. An algorithm for detecting and characterizing long-period R
ayleigh-wave arrivals has been developed and tested. The routine conti
nuously monitors all directions of approach to st station, in a manner
similar to beamforming. The detector is based on cross-powers between
the Hilbert-transformed vertical and rotated horizontal signals, so i
t is sensitive to both the power and polarization properties of the th
ree-component wave field. Elliptically polarized Rayleigh arrivals are
enhanced, while linearly polarized Love waves and body phases are sup
pressed. A test using one month of data from station ANMO demonstrated
that this technique can, with high reliability, detect Rayleigh arriv
als that are visible on the records. The measured arrival times and az
imuths are accurate enough to permit automated association of the dete
ctions to events in a bulletin.