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The solid‐state synthesis of perovskite BiFeO₃has been a topic of interest for decades. Many studies have reported challenges in the synthesis of BiFeO₃from starting oxides of Bi₂O₃and Fe₂O₃, mainly associated with the development of persistent secondary phases such as Bi₂₅FeO₃₉(sillenite) and Bi₂Fe₄O₉(mullite). These secondary phases are thought to be a consequence of unreacted Fe‐rich and Bi‐rich regions, that is, incomplete interdiffusion. In the present work, in situ high‐temperature X‐ray diffraction is used to demonstrate that Bi₂O₃first reacts with Fe₂O₃to form sillenite Bi₂₅FeO₃₉, which then reacts with the remaining Fe₂O₃to form BiFeO₃. Therefore, the synthesis of perovskite BiFeO₃is shown to occur via a two‐step reaction sequence with Bi₂₅FeO₃₉as an intermediate compound. Because Bi₂₅FeO₃₉and the γ‐Bi₂O₃phase are isostructural, it is difficult to discriminate them solely from X‐ray diffraction. Evidence is presented for the existence of the intermediate sillenite Bi₂₅FeO₃₉using quenching experiments, comparisons between Bi₂O₃behavior by itself and in the presence of Fe₂O₃, and crystal structure examination. With this new information, a proposed reaction pathway from the starting oxides to the product is presented.