The single crystals of four vanadyl(1V) phosphate hydrates A(VO)2(P04)2.4H20 (A = Co, Ca, Sr, Pb) were grown hydrothermally at 230 OC and were characterized by single-crystal X-ray diffraction and thermal analysis. Crystal data: Co(V0)2(P04)2.4H20, tetragonal, Mlmmm, a = 6.264 (1) A, c = 13.428 (4) A, V = 526.9 (2) A3, Z = 2, and R = 0.0527; Ca(V0)2(P04)2.4H20, triclinic, P1, a = 6.3484 (8) A, b = 6.350 (1) A, c = 6.597 (1) A, a = 106.81 (2)O, ,8 = 94.09 (1)O, y = 90.02 (1)O, V = 253.86 (8) A3, Z = 1, and R = 0.0221; Sr(VO)2(P04)2.4Hz0, monoclinic, Cc, a = 9.026 (2) A, b = 9.010 (3) A, c = 12.841 (3) A, ,8 = 100.19 (2)O, V = 1027.8 (1) A3, Z = 4, and R = 0.0350; Pb(VO)2(P04)2.4H20, monoclinic, Cc, a = 9.030 (3) A, b = 9.021 (2) A, c = 12.874 (4) A, ,8 = 100.16 (2)O, V = 1032.3 (5) A3, Z = 4, and R = 0.0307. All four structures contain layers of vanadiumphosphorus oxide with the water molecules and divalent metal cations between the layers. The layer is a 4-connected net in which corner-sharing vanadium oxygen polyhedra and phosphate tetrahedra alternate. In Co(V0)2(P04)24H20 the vanadium is 5-coordinated in form of square pyramids. In the Ca, Sr, and Pb compounds, the vanadium oxygen polyhedra are distorted octahedra. The Co compound contains units of linear V=O-Co-O=V.The structure of the Ca compound reported in this work is a triclinic polymorph of the rare mineral sincosite. The Sr and Pb compounds are isostructural. The four structures are discussed along with the parent VOP04.2H20.