Absorption spectra of Co(II)-chloride and bromide complexes have been taken in the UV-visible-NIR region, at temperatures from 25 to 90°C. The octahedral absorption bands have been resolved into components by fitting to Gaussian distribution functions, and the resolved bands have been assigned to ligand-field transitions using Tanabe-Sugano diagrams. The ligand-field-splitting energies, 10 Dq, were obtained for both chloro- and bromo-cobaltous complexes. These data were then used to estimate the average chloro-ligation number at each temperature and the chloride concentrations. At room temperatures and low halide concentrations, essentially only octahedral (6-fold) complexes exist. As the temperature is raised or, especially, as the ligand concentration increases, the complexes undergo a transformation from an octahedral to a tetrahedral (4-fold) configuration. A combination of graphical and numerical methods has been used to determine the stability constants. In the numerical treatment, activity considerations have been incorporated throughout. Based on these stability constants, the thermodynamic data, i.e. enthalpy, entropy and free energy changes, were calculated for all complexation reactions. It was found that the formation of both the first octahedral complex and the sole tetrahedral complex are endothermic. The favourable free energy changes for these reactions are due to gains of entropy inasmuch as they are hard-hard interactions, showing an electrostatic bonding character. The tetrahedral complexes exhibit a greater degree of electrostatic bonding than the first octahedral complex. The other octahedral complexes are extremely weak and do not show typical hard-hard or soft-soft interactions. The octahedral-tetrahedral transformation is strongly favoured by an increase in temperature or halide concentration or both. Thermodynamic calculations suggest that higher halogenated octahedral complexes and, to a lesser extent, Co(H 2O) 6 2+ are selectively converted to the tetrahedral complex, Co X 4 2−. It is possible to factor total dissolved cobalt in a fluid into two terms, a free cobalt term and an enhancement term due to chloride complexation. Investigation of each of the terms shows that under typical, low-temperature hydrothermal conditions ( e.g. during the formation of red-bed type and Mississippi-Valley type deposits), several ppm cobalt can be dissolved in natural fluids, provided that a sufficient source of cobalt is present. For major cobalt mineralization to occur, environmental conditions which produce a high free cobalt term and very high salinities (>5 m at 90°C which give rise to large enhancement factors) are required, in addition to a sufficient source of cobalt.