The surface composition of two natural sphalerites of different iron and lead content has been determined under flotation-related conditions by X-ray photoelectron spectroscopy (XPS). Oxidation of the mineral samples in air-saturated alkaline solutions has been found to be very slow. In the presence of copper (II) species in solution, copper exchanges with zinc, and metal-deficient environments are formed in the sulfide lattice at the surface. Cyanide removes the copper and some sulfur from the surface, but a metal-deficient sulfide layer remains. Treatment of sphalerite with cyanide can also result in lead impurity in the mineral migrating to the surface to form lead cyanide and hydrated lead oxide. Zinc-oxygen species were detected at the surface of sphalerite that had been immersed in alkaline zinc solutions and washed with dilute sodium hydroxide before examination. Copper was found to diffuse to the surface when sulfur was deposited on sphalerite by air oxidation of hydrosulfide ions. The resulting surface was a metal-deficient sulfide rather than an overlayer of elemental sulfur.