We have modified the iron-containing layer silicate nontronite into a
magnetic sample by heat treatment at 900 degrees C for 5 minutes and s
tudied the properties of the sample by Mossbauer spectroscopy, X-ray p
owder diffraction and infrared spectroscopy. Mossbauer spectra obtaine
d in applied magnetic fields show that the majority of the iron is sit
uated in a ferrimagnetic phase, related to maghemite.