Azurite, Cu3(CO3)2(OH)2, has been considered an ideal example of a one-dimensional (1D) diamond chain antiferromagnet. Early studies of this material imply the presence of an ordered antiferromagnetic phase below TN ∼ 1.9 K while magnetization measurements have revealed a 1/3 magnetization plateau. Until now, no corroborating neutron scattering results have been published to confirm the ordered magnetic moment structure. We present recent neutron diffraction results which reveal the presence of commensurate magnetic order in azurite which coexists with significant magnetoelastic strain. The latter of these effects may indicate the presence of spin frustration in zero applied magnetic field. Muon spin rotation µSR reveals an onset of short-range order below 3K and confirms long-range order below TN .PACS numbers: 61.05. fm, 75.50.Ee, 65.40.De, 76.75.+i Despite the burgeoning volume of data on the natural mineral azurite and its magnetic properties, the precise details of its spin-ordered state and the microscopic exchange couplings remain contentious issues. Recently, strong magnetoelastic coupling has been observed in azurite indicating significant interdependence of structural and magnetic degrees of freedom 1 . This effect is reminiscent of the spin-Peierls cuprate system CuGeO 3 2 in which the distortion is thought to be due to competing antiferromagnetic (AFM) interactions. In contrast, the structural distortion in azurite coincides with a transition to a three-dimensionally ordered AFM state.Azurite, Cu 3 (CO 3 ) 2 (OH) 2 is a quasi-1D system and the first realization of the distorted diamond chain 3,4 . Here, Cu 2+ ions form a triangular arrangement of spin S = 1/2 moments which are arranged as chains propagating along the crystallographic b-axis. The diamond chain model has been extensively studied 5-9 , with the distortion implied by three inequivalent exchange couplings, J 1 = J 2 = J 3 . This model affords a host of exotic phases and quantum phase transitions, including exotic dimer phases 7-9 or M = 1/3 fractionalisation 10,11 .Azurite has a monoclinic crystal structure (space group P2 1 /c) with room temperature lattice parameters a = 5.01Å, b = 5.85Å, c = 10.3Å, and a monoclinic angle, β = 92.4 •12-14 . An NMR study initially revealed the AFM phase transition at T N = 1.86K 15 while magnetization measurements have indicated the presence of a distinct 1/3 magnetization plateau 3,4 . Long range magnetic order was also confirmed by ESR measurements revealing AFM resonance modes below 1.9K 16 . Additional stud-ies, including muon spin resonance, indicated that the magnetic phase transition at T N is of second order 17-20 .Recently, there has been some controversy over the effective dimensionality of azurite. Ab initio density functional calculations have suggested that there is sizeable magnetic exchange between the diamond chains 21 . Inelastic neutron scattering measurements exhibit dispersive magnetic excitations along the chain 22 , indicating that significant magnetic exchange is present in this ...