The western Alps are an active collision belt whose current stress field is inhomogeneous <M¿ller et al., 1992>. We report new seismological data which significantly improve our knowledge of this stress field. About 1600 earthquakes which occurred in the western Alps during the last 10 years were precisely located, and 79 new focal solutions were computed. The analysis of this database shows that widespread extension affects all the internal zones of the belt. To better constrain the associated stress regime, six stress tensors were computed using the Gephart and Forsyth <1984> method. They show that the current tectonics of the western Alps are contrasted with close variation in the stress regime (transpression to the front of the belt contrasting with extension in the core of the belt). The extensional direction is radial of the arcuate geometry of the belt and bounded outboard by the former thrust of the internal zones onto the external zone, suggesting extensional reactivation of this inherited crustal discontinuity. Such widespread extension within the inner part of an actually ongoing collision belt cannot be explained by simple collision-related tectonics. We propose that intrabelt buoyancy forces, such as those produced by a slab retreat or slab break-off, interfere with the boundary forces driven by the ongoing Europe-Africa convergence. ¿ 1999 American Geophysical Union