Fe1+xTe crystallizes in the tetragonal α‐PbO structure and is isostructural with FeSe which structurally is the simplest of the iron‐based superconductors. The crystal structure of Fe1+xTe consists of stacked square‐lattice layers of iron atoms that are tetrahedrally coordinated to tellurium. Fe1+x Te orders antiferromagnetically at low temperature and exhibits pressure‐induced phase transitions. Jørgensen and Hansen (pp. 2257–2264) studied the p,T‐phase diagram of Fe1.141Te by high‐pressure neutron powder diffraction using the D20 diffractometer at the Institut Laue‐Langevin, Grenoble. The phase diagram contains three phases with monoclinic, orthorhombic, and tetragonal symmetry. The transitions from the high‐temperature tetragonal phase to the monoclinic and orthorhombic phases take place at 57 to 63 K depending on the pressure and they are accompanied by the onset of magnetic order. The monoclinic phase has commensurate bicollinear antiferromagnetic order while the orthorhombic phase exhibits incommensurate antiferromagnetic order. The tetragonal phase is non‐magnetic at high temperature but orders ferromagnetically for p ≥ 2.16 GPa and T ≤ 68 K. The observed ferromagnetic ground state may be of importance for the understanding of the complex interplay between magnetism and superconductivity in Fe‐based systems.