The solubilities of iron(III) oxide, formula Fe 2 O 3 , and cobalt(II,III) oxide, formula Co 3 O 4 , have been determined in the liquid mixture, isobutyric acid + water, along the critical isopleth at temperatures above the upper critical solution temperature near 299 K. When plotted in van't Hoff form with ln s versus 1/T , the measurements of solubility, s, lie on a straight line for values of the temperature, T , in kelvin, which are sufficiently in excess of the critical solution temperature, T c . The sign of the slope, (∂ ln s/∂(1/T )), indicates that in the case of both oxides, the dissolution reaction is endothermic. When the temperature is within 1 K of T c , however, the slope departs from its constant value and appears to diverge toward negative infinity. The principle of critical-point universality predicts that a divergence in (∂ ln s/∂(1/T )) is to be expected for T near T c in those cases where the stoichiometry of the dissolution reaction involves both components of the solvent; moreover, the Gibbs-Helmholtz equation predicts that, if the heat of solution is endothermic, the sign of the divergence should be negative. Both of these predictions are confirmed by the solubilities of Fe 2 O 3 and Co 3 O 4 measured as a function of temperature along the critical isopleth of isobutyric acid + water.