Our simulations reveal specific pathways for ion passage through the protein shell and highlight the critical role of interactions between ions and charged residues on the internal surface of the nanocage. We observed spontaneous nucleation events that allowed us to identify key structural motifs involved in the early stages of mineral formation, in agreement with experimental data. Furthermore, the estimation of nucleation rates sheds light on the role of confinement on the formation of minerals in the protein nanocage. This work advances our understanding of biomineralization within ferritin, providing a molecular characterization of the interplay between the interaction between the internal surface of protein nanocages and mineral nucleation.