Maximum solubility of Sn4+ ions in the spin glass Fe2Ti1-xSnxO5 (pseud
obrookite) corresponds to x = 0.22(3) at T = 1250 degrees C, and Sn4ions appear to occupy only 4c octahedral sites amongst the 4c and 8f s
ites. According to EPR data, the observed spin glass transition temper
ature T-g depends on tin concentrations nonmonotonically. The T-g valu
es correlate with the measurement times typical of EPR and some other
methods. This correlation is well approximated by the empirical Vogel-
Fulcher law.