AbstractAn experimental cross‐hole and face‐to‐borehole in‐seam seismic survey was carried out at Invincible Colliery in the Western Coalfield of New South Wales. Objectives were to determine propagation characteristics of the Lithgow seam and to establish the infrastructure for seismic mapping hole‐to‐hole in Australia.The seam supports leaky P‐, S‐ and P‐SV‐modes. These modes propagate with group velocities (at 60 Hz) of 3.1, 1.5 and 1.2 km/s respectively. Particle motion polarization is well developed, as is dispersion of the SH‐mode. Attenuation rates are high. The seam is lossy (Qof approximately 20). Two prominent structures were mapped by mode conversion. One is believed to be a fracture zone, the other a zone of intense roof thrusting.The old workings and a minor strike‐slip fault, which intersected raypaths, were found to be relatively transparent to P‐ and S‐waves at 60 Hz.Telemetry delay and shot‐break timing errors of the exploder box are significant. The resulting traveltime scatter is reduced by means of a least‐squares “statics” procedure. The group velocity estimation algorithm (based on Fourier transform) yields dispersion characteristics which can be matched with theoretical results for a simple model of a coal seam waveguide.The experiment demonstrates the capability to retrieve in‐seam seismic data of diagnostic quality over an appreciable distance (2 km). The experience gained in both survey layout and data processing will be beneficial to future seam wa