Four different hydrated iron phosphates were prepared as pure crystalline powders by precipitation in aqueous solutions under controlled pH: strengite, FePO4.2H(2)O (Pbca; a = 9.8923(6) Angstrom, b = 10.125(1) Angstrom, c = 8.729(1) Angstrom); metastrengite I, FePO4.2H(2)O (Pbnm; a = 5.226(2) Angstrom, b = 10.026(3) Angstrom, c = 8.917(3) Angstrom); metastrengite II, FePO4.2H(2)O (P2(1)/n; a = 5.3276(3) Angstrom, b = 9.800(1) Angstrom, c = 8.7129(6) Angstrom, beta = 90.532(6)degrees); and spheniscidite, NH4(Fe-2(PO4)(2)OH.H2O).H2O (P2(1)/n; a = 9.808(3) Angstrom, b = 9.727(3) Angstrom, c = 9.866(3) Angstrom, beta = 102.85(2)degrees). Thermogravimetric analysis revealed slightly more than 2 H2O molecules per FePO4 for the first three compounds, the excess being considered as adsorbed on the powders' surface. Temperature-controlled X-ray diffraction allowed isolation and determination of the stability domains of a large number of FePO4 polymorphs which may, or may not, reabsorb H2O upon exposure to ambient air. All these phases, after careful optimization of the electrode preparation, may be reversibly reduced to similar to90% of their theoretical capacities within the 2-4 V vs Li+/Li region.