Summary. An expiosion is considered in an initially air-filled, underground spherical cavity to which is connected a long, cylindrical tunnel. The cavity and tunnel size are, taken together, equivalent in volume to a fully decoupled spherical cavity (in accordance with the Latter criterion). Calculations indicate that, when the air is at standard conditions, the shock speed in the tunnel, D, is of the same order as the sound speed in the surrounding rock medium, cL. Moreover, the blast wave is approximately quasi-steady, and can be represented by a simple analytical function. This in turn permits a closed form solution for the far-field seismic amplitude spectrum. It is found that the low-pass filtering effectiveness of the tunnel is largely diminished unless D/cL s 1. With air-filled cavities, and depending on the source-receiver orientation, the spectral amplitude can actually exceed significantly the equivalent volume-sphere result. For practical purposes, this means that unless the cavity and tunnel are initially evacuated, say with a steam ejector system, the high-frequency decoupling capability will be no better, and possibly worse, than a conventional spherical cavity of the same total volume.