High pressure-high temperature studies of the structural (zinc blendecinnabar) phase transitions were performed in. Hg1-xFexS mixed crystals (s < 0.1) using synchrotron radiation and multianvil X-ray diffraction press. Pressure investigations of the Hall effect and conductivity of crystals containing up to a few percent of Fe were also performed at 295 K and 77 K. It was demonstrated that Fe in β-ΗgS creates deep, localized donor state resonant with the conduction band.PACS numbers: 61.10. Gs, 64.60.My, 71.55.Gs Mercury sulphide is a II-VI semiconducting compound which crystallizes either in the cinnabar structure (α-HgS, wide gap semiconductor stable at ambient conditions) or in the sphalerite (zinc blende) type structure (metastable β-ΗgS, a zero-gap semiconductor). It is known that the phase transition α-β is observed at about 344°C at ambient pressure for pure mercury sulphide [1]. Twenty years ago it was demonstrated that the sphalerite type structure of HgS may be stabilized by a partial substitution of mercury by manganese [2]. Later, using the modified Bridgman method, big size, good quality monocrystals containing Mn, Fe, or Co were obtained [3]. In particular, Hg1-x FeS monocrystals were grown • for 0.02 < x < 0.11 in the last few years. On the basis of classical and quantum transport measurements it has been suggested that iron in β-ΗgS could create a deep, localized donor state resonant with the conduction band [3,4]. In particular, noticeable effect of low temperature mobility enhancement (well known from the previous investigations of similar II-VI semiconducting system: HgSe doped with Fe -see, e.g., [5]) was found in Hg1-x Fex S samples with the lowest possible Fe concentration (slightly below 2%) [3]. One of the necessary conditions to observe such effect is pinning at the Fermi energy to the resonant donor level