Rumanova meteorite which belongs to the H5 chondrite group was investi
gated for the first time using Fe-57 Mossbauer spectroscopy. In the ma
gnetic fraction the magnetite, troilite and iron-nickel alloys were id
entified. In the non-magnetic fraction, the silicate phases such as ol
ivine and pyroxene were found. The paramagnetic component containing F
e3+ ions corresponds probably to small superparamagnetic particles.