Scanning electron microscopy coupled with energy dispersive X-ray spectroscopy (SEM/EDS) and Raman spectroscopy have been used to determine the chemistry and mineral components of Ellicott meteorite. Mineral phases and interstitial matrix in the meteorite slab were detected using backscattered electron mode (BSE) and scanning electron microprobe (SEM) and were assessed from atomic proportions of constituent elements, obtained by the EDS analysis. SEM/EDS and Raman shift analyses of mineral phases showed that Ellicott meteorite is characterized by the predominance of Fe-rich (Fe, Ni) alloy kamacite and Ni-Co-rich magnetite. The Iron-nickel phosphide minerals that are called schreibersite and rhabdites along with rare gold have been detected within the kamacite groundmass of meteorite. The presence of Neumann lines, which appear as fine parallel lines running in (up to) four directions, indicates impact with another body. These lines are caused by twinning due to the postconsolidation compression. The chemistry, particularly the lesser content of Ni and texture of unusual abundance ribbons of the iron-phosphide rhabdites and schreibersite where the Widmanstatten texture disappears after the etching by nitric acid, suggests that the Ellicott meteorite is an iron meteorite, hexahedrite type, IIG group.