Hydrogen bonding in euchroite has been studied by means of low-temperature single-crystal X-ray diffraction (XRD) and solid-state density functional theory (DFT) calculations. The mineral is orthorhombic, P2 1 2 1 2 1 , a = 10.0350(8), b = 10.4794(8), c = 6.1075(5) Å, V = 642.27(9) Å 3 , and Z = 4. The structure has been refined to R 1 = 0.036 for 2436 unique observed reflections with |F o | ≥ 4σ F . DFT calculations were performed with the CRYSTAL14 software package. The basic features of the crystal structure of euchroite are the same as described by previous authors. There are two symmetrically-independent Cu sites octahedrally coordinated by O atoms. The CuO 6 octahedra are strongly distorted containing four short (1.927-2.012 Å) and two long (2.360-2.797 Å) bonds each, in agreement with the expected Jahn-Teller distortion of an octahedrallycoordinated Cu 2+ cation. There is one symmetricallyindependent As site that is tetrahedrally coordinated by four O atoms to form an arsenate oxyanion, AsO 4 3− . The structure is based upon chains of edge-sharing CuO 6 octahedra running parallel to [001]. The chains are linked by AsO 4 tetrahedra into a three-dimensional framework, which is stabilized by hydrogen bonds formed from OH and H 2 O groups. The coordinates of H atoms determined by single-crystal X-ray diffraction and those calculated using DFT are very similar. The distance Δ between experimental and theoretical H positions does not exceed 0.250 Å, except for the H72 site, for which Δ = 0.609 Å. The hydrogen bonding scheme in euchroite is rather complex and involves a combination of relatively strong two-center hydrogen bonds as well as few three-center (bifurcated) hydrogen bonds. The largest difference between the XRD and DFT results involves the H72 atom of the H 2 O7 molecule and can be assigned to the effect of temperature, which favors a strong linear hydrogen bond at 0 K (calculated) and a bifurcated three-center bond at 100 K (measured). The Cu-H 2 O configurations are bent for the H 2 O7 and H 2 O6 groups and are almost planar for the H 2 O8 groups.