The orthorhombic compound has been studied by powder and single-crystal neutron diffraction. Below K, the magnetic moments order in a double- [, ] collinear magnetic structure, whose unit cell consists of four orthorhombic units in the direction. The refinements show that this structure consists of (0 1 0) ferromagnetic planes stacked along , in which the moments are oriented parallel to (the easy anisotropy axis according to bulk magnetization measurements) and nearly equal in magnitude (). The alternating eight-plane sequence providing the best agreement to the data turns out to be that which yields the lowest exchange energy if one assumes antiferromagnetic near-neighbor exchange interactions with . With increasing temperature, the single-crystal measurements indicate the suppression of the component at K, supporting the idea that the anomalies previously observed around 2–2.5 K result from a squaring transition. In a magnetic field applied along the axis, the magnetic Bragg satellites disappear at T, in agreement with earlier measurements. Comparisons are made with related magnetic orders occurring in ( Ru, Os) and .