The characteristics of Mossbauer spectra for a sample of schorlomite are described in this paper. There are 7 fitting doublets, three of which are considered as anomalous absorptions and their origin may come front complex electronic processes occurring in the schor]omite. It has been found that the isomer shift (IS) of Fe~(3+) exhibits an apparent temperature effectin the mineral studied. The characteristics of Mossbauer spectra for a sample of schorlomite are described in this paper. There are 7 fitting doublets, three of which are considered as anomalous absorptions and their origin may may front front complex electronic processes occurring in the schor] omite. It has been found that the isomer shift (IS) of Fe ~ (3+) exhibits an apparent temperature effect in the mineral studied.