The mineralogy of saprolitic laterites has been characterised using X-ray diffraction, Fourier transform infrared spectroscopy, thermal analysis and X-ray fluorescence. The results showed that the ore consists mainly of nickel- and iron-substituted lizardite and minor quantities of magnetite. Several experiments were conducted to investigate the extraction of nickel and cobalt from lizardite at atmospheric pressure in acidic media as a function of particle size, sulphuric acid concentration, reaction time, temperature and liquid to solid ratio. Generally, as much as 69·6%Ni and 30·8%Co were extracted under the experimental condition of 10% (v/v) H2SO4, reaction temperature 90°C, reaction time 2 h, particle size 59·9% passing through 74 μm, stirring at 500 rev min–1 and liquid to solid ratio 3 mL g–1. Increased extraction of Ni and Co from lizardite with sulphuric acid could be obtained by introducing leaching additives such as ferric chloride (Ni leaching rate 74·8%, Co leaching rate 45·4%), organic acid (Ni leaching rate 76·3%, Co leaching rate 48·7%) and fluoride (Ni leaching rate 81·7%, Co leaching rate 52·3%).