Saturation magnetizations were measured on single crystals of TbFe
2, DyFe
2, Tb
0.27Dy
0.73Fe
2and TmFe
2. Over most of the temperature rang from 4 K to 300 K, these values are substantially larger than those measured earlier on polycrystals. The intrinsic magnetic anisotropies, K
1(0)\´s, as determined from magnetic fields required for saturation, are huge (

erg/ cm
3). For these highly magnetostrictive compounds, the magnetoelastic contribution to the anisotropy

is a significant fraction of the total anisotropy.