The new mineral species arsenmedaite, ideally Mn ²⁺ ₆ As ⁵⁺ Si ₅ O ₁₈ (OH), has been discovered in quartz veinlets in the braunite ore deposit of the Molinello mine, Graveglia Valley, Ne, Genova, Liguria, Italy. It occurs as orange-reddish prismatic crystals, up to 200 μm in length, with a vitreous lustre, associated with braunite, quartz, calcite, As-rich medaite, calcian rhodocrosite, talc, and ganophyllite. Electron microprobe analysis of arsenmedaite gave (in wt%): V ₂ O ₅ = 1.84, As ₂ O ₅ = 6.81, SiO ₂ = 38.75, CaO = 0.70, MnO = 50.28, H ₂ O _calc = 1.42, total 99.80. On the basis of ∑Me = 12 atoms per formula unit, the chemical formula of arsenmedaite is (Mn _5.89 Ca _0.10 ) _∑5.99 [(As _0.49 V _0.17 ) _∑0.66 Si _5.35 ] _∑6.01 O _17.69 (OH) _1.31 . The main diffraction lines are [d in Å (relative intensity) hkl]: 3.266 (100) 081, 3.159 (72) 052, 3.094 (82) 221, 2.963 (83) 091, 2.935 (79) 211, 2.788 (68) 072, and 2.612 (98) 082. The crystal-structure study gives a monoclinic unit cell, space group P2 ₁ /n, with a = 6.7099(3), b = 29.001(1), c = 7.5668(3) Å, β = 95.469(3)°, V = 1465.7(1) Å ³ , Z = 4. The crystal structure has been solved and refined to R ₁ = 0.062 on the basis of 3526 reflections with F _o > 4σ(F _o ) and 287 parameters. Arsenmedaite is isotypic with medaite. In its crystal structure, six-to seven-fold coordinated Mn-centred polyhedra form wavy ribbons linked to TO ₄ tetrahedra centred by Si and (As,V). Its formation is likely related to the late-stage circulation of As-and Mn-rich hydrothermal fluids during the final stages of the Alpine tectono-metamorphic evolution of the manganese ore deposits of Eastern Liguria.