The magnetic ground state of polycrystalline N'eel skyrmion hosting material GaVS has been investigated using ac susceptibility and powder neutron diffraction. In the absence of an applied magnetic field GaVS undergoes a transition from a paramagnetic to a cycloidal state below 13~K and then to a ferromagnetic-like state below 6~K. With evidence from ac susceptibility and powder neutron diffraction, we have identified the commensurate magnetic structure at 1.5 K, with ordered magnetic moments of on the V1 sites and on the V2 sites. These moments have ferromagnetic-like alignment but with a 39(8) canting of the magnetic moments on the V2 sites away from the V cluster. In the incommensurate magnetic phase that exists between 6 and 13 K, we provide a thorough and careful analysis of the cycloidal magnetic structure exhibited by this material using powder neutron diffraction.

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