A first-order transition is a type of phase change characterized by a discontinuity in the first derivative of the Gibbs free energy with respect to some thermodynamic variable, such as temperature or pressure. During this transition, there is a latent heat associated with the change, meaning that energy must be added or removed without changing the temperature of the system. Common examples include the melting of ice into water or the boiling of water into steam, where distinct phases coexist at the transition point.