In the present work, spontaneous magnetization is observed in the inverse magnetic susceptibility of La 0.7 Ca 0.3 MnO 3 and La 0.7 Ba 0.3 MnO 3 compounds above T C up to a temperature T * . From information gathered from neutron diffraction, dilatometry, and high-field magnetization data, we suggest that T * is related to the transition temperature of the low-temperature (high magnetic field) magnetic phase. In the temperature region between T * and T C , the application of a magnetic field drives the system from the high-temperature to low-temperature magnetic phases, the latter possessing a higher magnetization.