Results of an experimental investigation of the evolution of vibrator-induced, steady-state sinusoidal ground vibration are reported and interpreted as suggesting the nonlinear wave phenomenon known as Fermi-Pasta-Ulam recurrence. Uniform-amplitude (unmodulated) sinusoidal wavetrains were generated by a 4441 N electrodynamic vibrator, the vertical force being used, and the evolution of the wavetrains was monitored on the ground surface by eight vertical seismometers. Two locations, 6 m apart, were used to install the vibrator. The seismometers were aligned along three profiles: two for the first location of the vibrator (30 and 60 m long) and one for the second (73 m long). The wavetrain carrier frequency was varied from 7 to 14.65 Hz; its amplitude measured from 0.015 to 0.6 cm s −1 at 1 m from the source. Whenever a wavetrain was generated with a Mach number below some critical value (∼ 10 −5 at 1 m from the vibrator), it evolved in a recurrent manner. The Fourier spectra of the records show that, during the initial stage of evolution, an instability developed resulting in a dramatic growth of the second and third harmonics, whose appearance is attributed to ground nonlinearity ( harmonic generation), and their lower sideband components. As the instability effects reached their peak levels, the wavetrain seemed to be losing its coherence, often becoming strongly modulated ( self-modulation). With increasing propagation distance, however, the energy gradually returned to the carrier component, and the wavetrain demodulated, recovering its original (uniform and coherent) form ( recurrence). Despite some important peculiarities, the unstable wavetrain evolution observed is believed to belong to the class of nonlinear wave phenomena known as Fermi-Pasta-Ulam recurrence. Since, by theory, recurrence involves solitons, the results also imply the existence of seismic solitons.