Abstract-Silicate glass system rich in Fe 2 + and Fe3+ with their various molar ratio is prepared, and the magnetic behaviors are studied systematically. The glasses basically behave as superparamagnet, which is attributable to deposited magnetite clusters. As the temperature drops, however, drastic shift of the field for ESR absorption as well as ferromagnetic type Curie-Weiss law in the dc susceptibility are observed. The novel characteristics is revealed to be caused by magnetic boundary intemction between the cluster and the surrounding amorphous region. As for the specimens with modemte component region (ratio from 0.39 to 0.66 ofFe 2 + to total Fe ions), the shifting ESR signal also shows an anomaly around lOOK caused by Verwey transition of magnetite, indicating that Verwey transition occurs even in the super fine scale about 40-55 A.