Cu-exchanged mordenite (MOR) is a promising material for partial CH₄ oxidation. The structural diversity of Cu species within MOR makes it difficult to identify the active Cu sites and to determine their redox and kinetic properties. In this study, the Cu speciation in Cu-MOR materials with different Cu loadings has been determined using operando electron paramagnetic resonance (EPR) and operando ultraviolet-visible (UV-Vis) spectroscopy as well as in situ photoluminescence (PL) and Fourier-transform infrared (FTIR) spectroscopy. A novel pathway for CH₄ oxidation involving paired [CuOH]⁺ and bare Cu²⁺ species has been identified. The reduction of bare Cu²⁺ ions facilitated by adjacent [CuOH]⁺ demonstrates that the frequently reported assumption of redox-inert Cu²⁺ centers does not generally apply. The measured site-specific reaction kinetics show that dimeric Cu species exhibit a faster reaction rate and a higher apparent activation energy than monomeric Cu²⁺ active sites highlighting their difference in the CH₄ oxidation potential.