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The cation distribution of MnxZn1-xFe2O4 (x = 0, 0.1, 0.2, 0.4, 0.6, 0.8, 0.9, 1.0) has been determined by neutron diffraction. The fraction of the Mn2+ ions in the tetrahedral sites is correlated to the variation of the lattice parameter with x. It is concluded from the measurements that zinc ferrite is a completely normal spinel and that the Mn2+ ions only occupy the tetrahedral sites up to x = 0.6.