Around 20 years ago, experimental investigations were conducted ob the influence of external pressure on the destructive action of an explosion.Since interest in the problem has again recently cropped up, in connection with oll and gas well stimulation this time [i, 2], it is meaningful Co analyze the experimental results obtained, and even more so, since they were not published completely in their time.We present here the results obtained i~ the Hydrodynamics Institute of the Siberian Branch of the Academy of Sciences of the USSR [3].,The tests were conducted in cylindrical Plexiglas blocks with height equal to the dlam~ eter. The specimen dimensions were 7 and 15 cm. Lead azide of 0.l-g mass for smalland 0o3-g mass for the large specimens was used as explosive.The charge was placed at the specimen center through a 6-~n-diameter axial hole, which was then filled with liquid styracryl. After polymerization, the physical properties of this latter are in agreement with the properties of organic galss. The specimens were placed in a hlgh-pressure chamber.The first series of tests (with the large specimens) were conducted in a ch-mber fabricated from an instrument shaft and having an organic glass viewing window. Water was the working fluid. The pressure varied in the 0.i (l atm) to 70-MPa range. High-speed filming of the destruction zone development (darkening) in the material was executed in the frame-by-frame mode with an SFR camera. Drawn copies of the movie frames at 32-~sec time intervals are presented in Fig. 1 for 0.i-, 9-, and 20-MPa pressures.In certain cases the development of isolated cracks could be traced.The trajectories R(t) of a conical crack developing from the bottom of a well, or more accurately, from the angular stress concentrators being formed as a result of the drilling, are shown in Fig. 2 for different pressures. Let us note that if the angular concentrators are removed after the drilling (for example, to treat the bottom of the hole wlth dichlorethane), then no conical crack is formed.Visual observations and photography of the specimens after the explosion and reduction of the pressure showed that the size of the destruction zone does not change upon diminution of the pressure from working to atmospheric. This circumstance permitted going over to a closed chamber in the research, where there was the opportunity to raise the external pressure substantially, to 400 MPa. Specimens of 8-cm dimension with a 0.l-g mass charge could here be used. A mixture of kerosene and machine oil was the working fluid o