The results of a set of experiments designed to delineate the nucleation rate, supersaturation, temperature surface for the system CaSO 4 •2H 2 O/H 2 O are reported. The data were obtained using the droplet technique coupled with in situ generation of SO 4 2− under the conditions that dS/dt was large during the early part of the induction period and it was zero during the actual nucleation events. The observed shape of the surface is compared with that suggested by the classical theory of nucleation and differences are commented on. The critical parameters important in classical nucleation theory are reported.