Hydrogen evolution and oxygen reduction as a function of pH of the electrolyte have been investigated for a-Fe,O, powders and colloids by means of a solar simulator. The discrete particle dimensions and surface dynamics of iron oxide seem to be the dominant factors leading to H, generation despite the unfavourable position of the conduction band in Fe,O,. Evidence is presented that photo-uptake of 0, occurs in a-Fe,O, suspensions.