Yes. All iron sulfate complex with water until all the binding sites are filled up.
In this case you get an octahedral complex that can be written as ##[Fe(H_2O)_6]SO_4## or drawn as:
where the oxygens on the waters point towards the iron.
A common name for it is Ferrohexahydrite. The scientific name for this would be either hexaaquairon(II) sulfate or iron(II) sulfate hexahydrate.
You can call ##Fe^(2+)## a ##d^6## transition metal in the context of Crystal Field Theory.
The waters are known as the ligands in this metal-ligand complex. Water is a relatively weak-field ligand meaning that it generates only small repulsive forces that do not cause much splitting of the ##d##-orbital energy levels (as a ligand approaches to form a metal-ligand interaction repulsive forces would decrease the stability of the interaction thereby creating a difference in the energy levels of the most significantly different orbital shapes).
That means that the energy levels of the ##d_(x^2 – y^2)## and ##d_(z^2)## orbitals are not very high above the energy levels of the ##d_(xy)## ##d_(xz)## and ##d_(yz)## orbitals. Therefore this octahedral complex gives rise to high-spin state in which electrons are likely to fill all the ##d##-orbitals one at a time then double up.