Found on a specimen in the mineral collection of the National Museum of Wales, no. NMW 27.111.GR414, from the Aberllyn mine, Llanrwst mining field, North Wales, with hydrozincite on a breccia cemented by sphalerite, quartz, calcite, and ankerite. Atomic absorption and TGA analyses gave ZnO 37.8, CuO 22.0, SO₃ 14.9, H₂O 24.5, total 99.2%, corresponding to (Zn_2.50 Cu_1.49)_Σ3.99 S_1.00 O₇·7.32 H₂O on the basis of total O = 7 in the anhydrous part. The ideal formula is (Zn,Cu)₄SO₄(OH)₆·4H₂O where Zn > Cu. It is hexagonal a 8.29, c 10.50 ± 0.01 Å, possible space groups P6, P¯6, P6/m, P622, P6mm, P¯6m2, P¯62m, and P6/mmm. Isomorphous with synthetic Zn,SO₄(OH)₆6·4H₂O and (Zn,Cu)₄SO₄(OH)₆·4H₂O. Strongest X-ray powder diffractions are: 10.59(100)0001, 5.31(15)0002, 4.15(25)11¯20, 2.71(42)21¯30, 2.63(41)21¯31,0004, 2.41(22)21¯32, 1.57(23)32¯52, 1.55(20)41¯51. Namuwite is pale sea-green in colour, lustre pearly, streak very pale green, H (Mohs) 2. Cleavage {0001}, perfect. Density (g/cm³) 2.77 (meas.), 2.81 (calc. on the normalized empirical formula). It is optically uniaxial, sign not determined owing to the extremely low birefringence. Refractive index n = 1.577(5)(NaD). The mineral and name have been approved by the Commission on New Minerals and Mineral Names, IMA.