The aqueous speciation of iron(III)-tris(pyridylmethyl)amine (TPA) complexes was determined from potentiometric titration data, and the overall formation constants (beta) for relevant species were calculated. At pH < 3 the mononuclear complex [Fe(TPA)](+3)(aq) predominates (log beta = 10.75(15). Above pH 3 Fe3+-OH2 hydrolysis produces the mu-oxo dimer [Fe-2(mu-O)(TPA)(2)(H2O)(2)](+4) (1a; log beta = 19.91(12)). This species is a diprotic acid with the conjugate bases [Fe2(mu-O)(TPA)(2)(H2O)(OH)](+3) (1b; log beta = 15.53(6)) and [Fe-2(mu-O)(TPA)(2)(OH)(2)](+2) (1c; log beta = 10.27(7)). The pKas of 1a are 4.38(14) and 5.26(9). Compounds 1a-c quantitatively oxidize hydroquinone to benzoquinone with concomitant formation of 2 equiv of Fe(II). Kinetic and spectroscopic data at pH 5.6 are consistent with rapid equilibrium formation of a diiron(III)-phenoxide intermediate followed by rate-controlling electron transfer. The equilibrium constant for the formation of the intermediate complex is 25(3) M-(1), and the rate constant for its decomposition is 0.56(9) s-(1). A kinetic isotope effect of kH/kD = 1.5 was determined from proton inventory experiments in mixed H/D media. The mu-oxo-diiron(III) phenoxide intermediate is hydrolyzed in a pH dependent process to form a mononuclear iron(III)-phenoxide, which complicates the kinetics by introducing a fractional dependence on total iron(III) concentration in the pH range 4.1-5.2. The pH-dependent cleavage of mu-oxo-diiron(III)-phenoxides was investigated with phenol, a redox-inert proxy for hydroquinone. The addition of phenol to 1 facilitates acidic cleavage of the mu-oxo dimer to form [Fe(TPA)(OPh)(H2O)](+2), which becomes the dominant iron(III)-phenoxide as the pH decreases to 4. The 2-naphtholate analogue of this intermediate, [Fe(TPA)(2-naphtholate)(OCH3)]ClO4 (6), was characterized by single-crystal X-ray diffraction (C29H28FeN4O2,ClO4; P21; a = 13.2646(2) A, b = 15.2234(3) A, c = 13.7942(3) A; Z = 4).