The magnetic ground state in the double perovskite system Sr 2-x Ca x CoOsO 6 changes from an antiferromagnet (x = 0), to a spin glass (x = 1), to a ferrimagnet (x = 2) as the Ca content increases. This crossover is driven by chemical pressure effects that control the relative strength of magnetic exchange interactions. The synthesis, crystal structure, and magnetism of SrCaCoOsO 6 While this change may seem minor it has a profound effect on the magnetism, changing the magnetic ground state from antiferromagnetic in Sr 2 CoOsO 6 (T N1 = 108 K, T N2 = 70 K), to a spin glass in SrCaCoOsO 6 (T f1 = 32 K, T f2 = 13 K), to ferrimagnetic in Ca 2 CoOsO 6 (T C = 145 K). In the first two compounds the observation of two transitions is consistent with weak coupling between the Co and Os sublattices.2