The magnetic behavior of FeCl2 . H2O is examined for the first time. T
he susceptibility exhibits a sharp peak at 20.4 K which may be cusp-li
ke, and which is very different from the antiferromagnetic maximum in
the dihydrate. Field-cooled and zero-field-cooled susceptibilities dif
fer at low temperatures but become coincident near 24 K. The thermorem
anent magnetization shows time dependence below 20 K. Competition betw
een ferromagnetic and antiferromagnetic interactions in the dihydrate
is presumably accentuated, and randomized, on removing half the waters
, leading to a spin glass.