The surface areas of natural ores, electrolytic, chemical, and synthetic hydrous MnO2 samples were determined by both low-temperature nitrogen gas adsorption and water vapor adsorption at 25~ using the B.E.T. adsorption isotherm relationship. These various types of manganese dioxides have distinctly different surface areas as determined by the two methods. The water content retained at ll0~ and corrected total water content were found to be surface area dependent. The synthetic hydrous MnO 2 samples occupy a unique position due to their high water content.