Structural properties of Pb-exchanged zeolites are of interest because of their applications in environmental remediation and in industrial processes. In this study, we report on a Pb-exchanged stellerite (Pb-STI), with particular focus on the cationic species, which form inside the zeolitic pores as a result of the exchange experiments. The produced zeolite had chemical composition Pb 13.4 (OH) 10 Al 17.4 Si 54.6 O 144 ∙38H 2 O, indicating that Pb was uptaken in form of [Pb(OH) x ] (2-x) species. The STI framework maintained the Fmmm space group characteristic of the type material. However, the extraframework occupants, Pb 2+ , H 2 O and OH − , were characterized by a strong positional-disorder. The latter was resolved and interpreted combining Extended X-ray Absorption Fine Structure (EXAFS) analysis with Molecular Dynamics (MD) simulations. On average, Pb 2+ ions are coordinated by 2 OH − and 1H 2 O at distances <2.5 Å, whereas bonds to framework oxygen-atoms were found only at longer distances (>2.8 Å). Pb 2+ adopts mainly a sided distorted coordination, indicating a stereochemical activity of the lone pair electrons. The obtained results were compared with those of other mono-cationic forms of STI zeolites. Based on the analysis of the framework distortion experienced after the incorporation of different metal ions, considerations are drawn on the potential effect of Pb 2+ on the thermal stability of STI framework type zeolites. • A STI zeolite was Pb-exchanged in 0.5 M Pb(CH 3 COO) 2 solution at pH = 5-6. • No framework distortion from the Fmmm symmetry was observed. • The EF species (Pb 2+ , OH − , and H 2 O) were highly disordered in the cavities. • Pb 2+ is sided coordinated by OH − and H 2 O. • No significant interactions occur between Pb and framework oxygen.