Copper sulfide crystallizes in the hexagonal crystal system, and this is the form of the mineral covellite. There is also an amorphous high pressure form as a Cu(II) compound would have a d9 configuration and be expected to be paramagnetic. indicate that
all of the copper atoms have an oxidation state of +1. This contradicts a formulation based on the crystal structure and obeying the
octet rule that is found in many textbooks (e.g.) describing CuS as containing both {{chem2|Cu^{I} }} and {{chem2|Cu^{II} }} i.e. . An alternative formulation as was proposed and supported by calculations. The formulation should not be interpreted as containing radical anion, but rather that there is a delocalized valence "hole".{{cite journal
Electron paramagnetic resonance studies on the precipitation of Cu(II) salts indicates that the reduction of Cu(II) to Cu(I) occurs in solution.{{cite journal ==See also==