Ferricoronadite is a lead mineral discovered in 2016 by Chukanov et al. near Nezhilovo, North Macedonia. Its simplified elemental formula is Pb(Mn<sub>6</sub><sup>4+</sup>Fe<sub>2</sub><sup>3+</sup>)O<sub>16</sub>, and it is found in a matrix of zinc-dominant spinels. Ferricoronadite is named as an analogue of coronadite.