The crystal structures of natural huemulite from the West Sunday mine, Utah, USA, and synthetic huemulite, Na4Mg(V10O 28)·24H2O, have been solved and refined to R 1 = 0.0313 (for 3535 unique F0 > AσF reflections) and 0.0246 (for 3672 unique F0 > 4σF reflections), respectively. Huemulite is triclinic, space group P1̄, Z = 1; unit-cell dimensions of the natural sample are a 9.0453(2), b 11.3337(3),c 11.7372(8) Å, α 105.223(7), β 97.383(7), γ 100.790(7)°, V 1120.30(9) Å3, whereas those of the synthetic sample are a 9.0425(2), b 11.3303(2), c 11.7353(8) Å, α 105.222(7), β 97.377(7), γ 100.791(7)°, V 1119.47(8) Å3. The structure consists of decavanadate oxyanions (V10O28) 6- linked via an interstitial complex composed of isolated [Mg(H 2O)6]2+ o...