A stable Sr 4 fe 6 o 13 was prepared as small crystallites by auto-combustion of a sol-gel in air followed by annealing the later at pertinent temperatures. A green sample, as annealed at elevated temperatures, yields a single Sr 4 fe 6 o 13 phase of tailored magnetic properties. the structural, morphological, magnetic and electrical properties were investigated by X-ray diffraction, transmission electron microscopy, vibrating sample magnetometer, and broadband dielectric spectrometer. Hard magnetic Sr 4 fe 6 o 13 properties arise with saturation magnetization M s = 12.4 emu/g, coercivity H c = 3956.7 Oe and squareness 0.512. Studies made at low temperatures reveals M s decreasing on increasing temperature from 17.5 emu/g at 85 K down to 12.4 emu/g at 305 K, while H c rises from 1483 Oe at 85 K to 1944 Oe at 305 K. The ac-conductivity follows the Jonscher relation. The dc-conductivity at high temperatures/ low frequencies exhibits a plateau and it depends linearly on a characteristic frequency according to the Barton-nakajima-namikawa) relation. Perovskites are compounds of a structural formula ABC 3 , where A represents a rare earth, alkaline earth, alkali or large ions such as Pb 2+ , Bi 3+ , B represents a transition metal ion and C represents O, Fl, Cl, I etc 1. A cation may be monovalent like Li, Na, K, divalent like Ca, Ba, Sr or trivalent like La, Nd, Pr, which is cubo-octahedrally coordinated to 12 O 2− ions, while B cation, such as Ti, Ni, Fe, Co, or Mn is octahedrally coordinated to 6 O 2− ions 2. Recently, several investigations performed on a Sr-Fe-O structure reveal its amazing structural and physical features such as cheap price, high magnetic anisotropy, high Curie temperature, a significant magnetization of saturation and remarkable chemical and corrosion resistance 3. The reason certainly presented by oxygen-lacking perovskites and by Ruddlesden-Popper (RP) type structure that possess a desirably negative magnetoresistance (-ve MR) 4-7. A Sr-Fe-O system includes many types of perovskites and perovskite derivatives of widely varied crystalline and magnetic features 8-12. These types of substances are constructed based on a K 2 NiF 4 shape and involve slab segments of SrFeO 3 and SrO, where SrFeO 3 is resulting from a KNiF 3 cubic perovskite of K 2 NiF 4 , and SrO is matching to a NaCl-class KF 8. They characteristically contain paramagnetic Fe 4+ ions. In particular, a stoichiometric compound Sr 4 Fe 6 O 13 has a construction of a perovskite or its derivatives 8. It is observed that a Sr 4 Fe 6 O 13±δ construction is a highly stable single-phase compound and it exhibits significant conductivity of combined-ions and electrons types 13. That is composed of altered sections through a Sr-Fe-O layer (b-axis) and dual slabs of FeO in FeO 5 polygons 14-16. As a result, it owes an anisotropic shape in it conducts through O 2− ions and vacancies across the a-c planes 17. Actually, creation of O 2− empty sites and interstitials develop non-perovskite slabs in a Sr 4 Fe 6 O 13±δ phase keeps them in a broad a...