The stunning blue-green color of the water at Niagara Falls is a result of the immense power of erosion and the specific mineral composition of the Great Lakes basin. As the massive volume of water flows from Lake Erie toward Lake Ontario, it carries a high concentration of "rock flour," which consists of finely ground particles of limestone, shale, and sandstone. When sunlight hits the water, these suspended minerals absorb most of the spectrum but scatter the blue and green wavelengths back to our eyes. Additionally, the sheer depth and speed of the water contribute to its clarity and hue. It is estimated that 60 tons of dissolved minerals are swept over the falls every minute. This natural phenomenon is most vibrant during the spring and summer months when the flow is at its peak. In 2026, visitors can still observe that the water is notably clearer and "bluer" than many other large river systems, as the Great Lakes act as giant settling basins that trap heavier sediments before the water reaches the Niagara River.