A new experimental method has been devised that directly determines th
e group velocities of surface acoustic waves. A point source and a poi
nt detector are employed to measure the ultrasonic transmission across
a solid surface as a continuous function of the propagation direction
. Results for single pulses give the times-of-flight for both Rayleigh
surface waves (RSW's) and pseudo-surface-waves (PSW's). Calculations
and measurements of the group velocities of the surface waves on silic
on show some unanticipated behavior: fluid loading qualitiatively chan
ges the group velocity curves for both RSW and PSW. In particular, the
RSW branch gains an additional component which we denote here as an i
nduced Rayleigh wave (IRW). If a wave train is employed in the experim
ent, the analog of phonon focusing is observed for the ultrasonic wave
s, modified by ''internal-diffraction'' effects. Systematic measuremen
ts of the wave intensities on silicon as a function of propagation dis
tance are consistent with expected acoustic losses into the surroundin
g water: the attenuation length of a wave depends on the mode and freq
uency. A survey of surface-wave images on other crystals is included i
n this study.