PrRu2Si2 shows ferromagnetism below 14 K with the ordered moment of 2.7μB. It exhibits an enormous magnetic anisotropy at 4.2 K with the anisotropy field of about 400 T. We have attrributed the magnetism of PrRu2 Si2 to the Pr 3 + ions. Thus we performed calculations of the fine electronic structure of the Pr 3+ ion in the tetragonal symmetry, relevant to PrRu2Si2, taking into account crystal-field and inter-site exchange interactions. Our calculations reproduce well the zero-temperature moment, the single-crystalline magnetization curves, and giant anisotropy field as 400 T. The magnetocrystalline-anisotropy energy K1 of 59 J/cm 3 is the largest known anisotropy -the anisotropy energy of the Nd 2 Fe 14 Β supermagnet amounts to 12.5 J/cm 3 only. Unfortunately, this giant anisotropy is confined to low temperatures only which prohibits its technical applications in the permanent-magnet industry.PACS numbers: 71.20.Eh PrRu2Si2 exhibits a giant magnetocrystalline anisotropy about 400 T [1, 2]. The aim of this contribution is to find the origin of this giant anisotropy, in the current literature as the source of the anisotropy three main factors are mostly discussed [1]: the anisotropic exchange, the hybridization, and the single-ion mechanism. We are by years in favour of the single-ion mechanism [3,4], via the crystal-field effect, of the magnetocrystalline anisotropy and it was very intriguing that the authors of Ref. [1] have claimed that such big anisotropy cannot be obtained as the crystal-field effect. Moreover, our interest to PrRu2Si2 has raised as the preceding compound, CeRu 2 Si2 , exhibits the pronounced heavy-fermion phenomena. It turns out that we can provide the crystal-field explanation for this giant magnetocrystalline anisotropy, that provides also a quite consistent description of other magnetic and electronic (m-e) properties.PrRu2Si2 is an intermetallic compound. It crystallizes in a tetragonal structure of ThCr2Si2-type and exhibits the ferromagnetic ordering below 14K [1,2,5,6]. The magnetization curves measured on a single-crystalline sample [1], which reveal this giant magnetocrystalline anisotropy, are shown by experimental points in (767)