Oxygen evolution reaction (OER) through water oxidation under acidic conditions catalyzed by first-row transitionmetal-based compounds remains a challenge in artificial photosynthesis. A critical issue for OER under acidic conditions is the solubility of first-row transition-metal compounds during the reaction. This study investigates the silicate-stabilized Mn oxide for OER under acidic conditions (H 2 SO 4 (0.10 M)). Compared to Mn oxide, the silicate-stabilized Mn oxide is significantly more stable under acidic conditions , with an overpotential of 457 mV for the onset of OER. The Mn oxides forming in the absence and presence of silicate groups are α-Mn 2 O 3 and α-MnO 2 , respectively. For the Mn oxides forming in the presence of silicate groups, the corresponding current densities of 1 and 10 mA/cm 2 are recorded at 527 and 640 mV, respectively. Silicate-stabilized Mn oxide was characterized by several methods before and after OER. The 29 Si NMR spectrum for silicate-stabilized Mn oxide shows that the Si− O groups chemically bonded to Mn ions. The scanning transmission electron microscopy shows small 2−10 nm particles of Si−O compound in silicate-stabilized Mn oxide, especially Si−O, to stabilize the higher-indices facets of the Mn oxide crystallites. X-ray absorption spectroscopy confirms that the predominant structure for silicate-stabilized manganese oxide is α-MnO 2 , with di-and mono-μ-oxo-bridged Mn atoms. After prolonged oxygen evolution, a certain fraction of the mono-μ-oxo bridges disappears for silicate-stabilized manganese oxide. Adding silicate to Mn oxide is a low-cost and environmentally friendly procedure to increase the stability of Mn oxide toward OER under acidic conditions. Thus, our procedure is a clear improvement on current methods to stabilize Mn oxide for OER under acidic conditions.