Abstract. Given three transversal and sufficiently regular hypersurfaces in R 3 it follows from work of Bennett-Carbery-Wright that the convolution of two L 2 functions supported of the first and second hypersurface, respectively, can be restricted to an L 2 function on the third hypersurface, which can be considered as a nonlinear version of the Loomis-Whitney inequality. We generalize this result to a class of C 1,β hypersurfaces in R 3 , under scaleable assumptions. The resulting uniform L 2 estimate has applications to nonlinear dispersive equations.