Impurity scattering is found to lead to quasi-one dimensional nanoscale modulation of the local density of states in the iron pnictides and chalcogenides. This 'quasiparticle interference' feature is remarkably similar across a wide variety of pnictide and chalcogenide phases, suggesting a common origin. We show that a unified understanding of the experiments can be obtained by simply invoking a four-fold symmetry breaking dxz − dyz orbital splitting, of a magnitude already suggested by the experiments. This can explain the one-dimensional characteristics in the local density of states observed in the orthorhombic nematic, tetragonal paramagnetic, as well as the spin-density wave and superconducting states in these materials.The intriguing anisotropic electronic properties of iron pnictides [1] are reflected in transport measurements [2][3][4], optical conductivity [5], angle-resolved photoemission spectroscopy (ARPES) [6], and scanning tunneling microscopy (STM) [7]. It is not unexpected in a state having a broken four-fold rotational symmetry such as the spin-density wave (SDW) state or the orthorhombic 'spin nematic' state, but the lattice anisotropy does not explain the splitting of ≈ 60meV between the d xz and d yz orbitals [8,9]. The orbital splitting (OS) actually persists into the high temperature tetragonal phase [9]. This suggests that the OS, rather than the orthorhombic symmetry or magnetic order, could be the key player in electronic anisotropy. A similar OS exists in various phases [10][11][12][13][14][15] of the chalcogenide including the superconducting state. The energy scale of FeSe splitting, and its orbital character, has been contrasted with those of the pnictides, with some suggestions of a momentum dependent, i.e, non-uniform splitting. Unlike the pnictides where the degeneracy of bands is dominated mainly by d xz and d yz orbitals at X or Y points is lifted at low temperature, the OS for chalcogenides may also exhibit sign reversal. Some have reported it to be of entirely different nature, OS between d xz/yz and d xy [16,17].Valuable insight into electronic anisotropy can be obtained through the 'quasiparticle interference' (QPI) phenomena which basically probes the spatial variation of the local density of states (LDOS), due to impurities in the medium, using the spectroscopic imaging STM [18]. A remarkable characteristic of the QPI common to the SDW state, the orthorhombic nematic phase, and the tetragonal paramagnetic phase, in some of the pnictides is the occurrence of quasi-one dimensional real-space LDOS modulation with material dependent lengthscale [7,19,20]. Corresponding momentum-space structure in the form of almost parallel ridges are aligned along a direction reciprocal to the ferromagnetic direction in the SDW state, or b-axis in the orthorhombic phase for pnictides. Similar momentum-and real-space structures have been reported in superconducting phase of chalcogenides [11]. * dheeraj@postech.ac.kr † alireza@apctp.org This suggests a common origin of the anisotropy in the ele...