The nuclear quadrupole moment of the I π =3/2 − excited nuclear state of 57 Fe at 14.41 keV, important in Mössbauer spectroscopy, is determined from the large-scale nuclear shell-model calculations for 57 Fe and also from the electronic ab initio and density functional theory calculations including solid state and electron correlation effects for the molecules Fe(CO)5 and Fe(C5H5)2. Both independent methods yield very similar results. The recommended value is 0.16(1) eb. The NQM of the isomeric 10 + in 54 Fe has also been calculated. The new value (0.5 eb), consistent with the perturbed angular distribution data, is by a factor of two larger than the currently recommended value.21.10. Ky, 21.60.Cs, 31.15.Ar, 31.30.Gs, 76.80.+y, 27.40.+z Mössbauer spectroscopy of 57 Fe plays an important role in the structural determination of iron containing solid state compounds. In principle, the nuclear quadrupole moment (NQM) of the isomeric I=3/2 state in 57 Fe can be determined from Mössbauer data; however, the analysis requires the calculation of the electric field gradient (EFG). As these atomic calculations are quite involved, studies employing different methods arrived at quite distinct results; the values of NQM in the range from -0.19 to +0.44 eb have been reported [1]. This quite unsatisfying situation could also not have been settled by nuclear structure calculations of the NQM as calculations within the nuclear shell model, the most reliable tool for such studies, had to be performed in strongly truncated model spaces and with rather untested effective interactions. In recent years, decisive progress has been achieved in both the atomic calculations of the EFG and in nuclear shell model studies.In 1995, Dufek and co-workers applied the density functional theory for a series of iron-containing solid state compounds. For 57 Fe they obtained a NQM of 0.16 eb [2], in contradiction with the previously accepted value of 0.082 eb obtained from Hartree-Fock (HF) EFG calculations [3] and from truncated nuclear shell-model calculations combined with the perturbed angular distribution data [4]. In subsequent work, Su and Coppens obtained a NQM value of 0.12(3) eb using Sternheimer-corrected EFGs [5]. In this Letter, we shall demonstrate that stateof-the-art nuclear and atomic physics calculations lead to the same NQM for the 57 Fe isomeric state, settling a long-standing controversial issue.We shall begin with the nuclear physics discussion. The nucleus 57 Fe has two low-lying 3/2 − states which are experimentally split by only 353 keV. To describe the structure of such nearly degenerate states is quite demanding. Clearly, the large-scale shell model is the method of choice. Due to recent progress in programming and hardware development, modern shell-model calculations based on microscopic effective interactions can handle configuration spaces that were prohibitively large only several years ago [6]. More specifically, modern diagonalization shell-model codes can now handle mediummass nuclei (A=50-60) in the middle of the...